1 Gompertz, Makeham, and Siler models explain Taylor's law in human - - PDF document
1 Gompertz, Makeham, and Siler models explain Taylor's law in human - - PDF document
1 Gompertz, Makeham, and Siler models explain Taylor's law in human mortality data 2 Research Article 3 Authors 4 Joel E. Cohen*, Christina Bohk-Ewald*, Roland Rau 5 * JEC and CBE contributed equally to the preparation of the manuscript. 6
Abstract 27 BACKGROUND 28 Taylor’s law (TL) states a linear relationship on logarithmic scales between the variance and the 29 mean of a nonnegative quantity. TL has been observed in spatiotemporal contexts for the population 30 density of hundreds of species including humans. TL also describes temporal variation in human 31 mortality in developed countries but no explanation has been proposed. 32 OBJECTIVE 33 To understand why and to what extent TL describes temporal variation in human mortality, we 34 examine whether the mortality models of Gompertz, Makeham, and Siler are consistent with TL. 35 We also examine how strongly TL differs between observed and modeled mortality, between 36 women and men, and between countries. 37 METHOD 38 We analyze how well each mortality model explains TL fitted to observed occurrence-exposure 39 death rates by comparing three features: the log-log linearity, the age profile, and the slope of TL. 40 We support some empirical findings from the Human Mortality Database with mathematical proofs. 41 RESULTS 42 TL describes modeled mortality better than observed mortality and describes Gompertz mortality 43
- best. The age profile of TL is closest between observed and Siler mortality. The slope of TL is
44 closest between observed and Makeham mortality. 45 The Gompertz model predicts TL with a slope of exactly 2 if the modal age at death increases 46 linearly with time and the parameter that specifies the growth rate of mortality with age is constant 47 in time. 48 CONCLUSIONS 49
TL describes human mortality well in developed countries because their mortality schedules are 50 approximated well by classical mortality models, which we have shown to obey TL. 51 CONTRIBUTION 52 We provide the first theoretical linkage between three classical demographic models of mortality 53 and TL. 54 55
- 1. Introduction
56 Taylor's law (TL) states that the logarithm of the variance of some nonnegative quantity is 57 approximately a linear function of the logarithm of the mean of that quantity, in multiple sets of 58
- bservations. TL describes the population densities of hundreds of species in ecology (Taylor 1961;
59 Kilpatrick and Ives 2003; Kendal 2004) and other nonnegative quantities in medicine (numbers of 60 metastases), epidemiology (cases of infectious diseases), genetics (numbers of single-nucleotide 61 polymorphisms), and many other fields (Eisler et al. 2008). In human demography, TL describes the 62 density (people per area) of Norway's population (Cohen, Xu, and Brunborg 2013) and the age- 63 specific force of mortality (henceforth, simply "mortality") in developed countries (Bohk, Rau, and 64 Cohen 2015). 65 As an empirical generalization, TL invites attempts at explanation. Why is there an approximately 66 linear relationship between the log of the temporal mean and the log of the temporal variance of 67 mortality in many developed countries? Is this empirical regularity in human mortality just a 68 coincidence or does it come from an underlying pattern or mechanism? Here we answer these 69 questions by comparing the completely empirical results of Bohk et al. (2015) with the results of 70 fitting three human mortality models: those of Gompertz (1825), Makeham (1860), and Siler (1979; 71 1983), which belong to the same family. We show that fitted mortality of these models obeys TL, 72 exactly or approximately. Hence these models provide a theoretical basis for TL in human 73 mortality. 74 Mortality models express mathematically the age schedule of mortality (that is, mortality as a 75 function of age) in a given year. Models differ in the number of parameters they use and in the age 76 ranges for which they model mortality well. The more parameters they use, the more flexibly they 77 can fit mortality at different ages, but the more difficult they are to analyze mathematically. 78 Gompertz' model (1825), with two parameters, is one of the most popular models in demography. It 79 assumes a linear increase in the logarithm of mortality with age. It usually describes well mortality 80
at ages 30 to 90 (so-called senescent mortality). The model of Makeham (1860) adds to Gompertz' 81 model an additional age-independent constant to represent non-senescent background mortality 82 effective at all ages. This improves the fit at some younger ages. The model of Siler (1979; 1983) 83 adds to the Makeham model an exponential decay in mortality to represent the decline in mortality 84 from infancy to childhood. 85 The main objectives of this study are to examine whether the models of Gompertz, Makeham, and 86 Siler are consistent with TL and can help to explain why and to what extent TL holds. In addition, 87 we examine how strongly TL differs between observed mortality and model mortality schedules, 88 between women and men, and between countries. 89 We base our analysis on empirical occurrence-exposure death rates, statistical analysis, and 90 theoretical explanations, and thus provide the first theoretical linkage between three classical 91 demographic models of mortality and TL: We show mathematically that the Gompertz model (the 92 simplest of the three models we considered) with linearly changing modal age at death and a 93 constant rate of growth of mortality with age predicts TL with a slope that is exactly equal to 2. As 94 the Gompertz model is a special case of the other two models, it is evident that the results from the 95 Gompertz model are also valid for certain parameter values of the more complex models of 96 Makeham and Siler. 97 Our analyses yield theoretical and empirical insights into the occurrence of TL in human mortality, 98 giving a comprehensive picture of the extent to which TL describes the temporal variance in age- 99 specific mortality in human populations. As we have confirmed TL to be a regular pattern (rather 100 than a coincidence) in human mortality, it can be validly applied in other demographic studies such 101 as generating and evaluating mortality forecasts. 102 In the remainder of this article, section 2 describes data and methods; section 3 presents results; and 103 section 4 summarizes the main findings. Appendices 1 and 2 give theorems, mathematical proofs 104
and approximations of TL for the Gompertz and Makeham models, respectively. Supplementary 105 material (online) includes estimates of model parameters, figures, and descriptive files. 106
- 2. Data and methods
107 We extracted deaths and life-years of exposures to the risk of death by single year of age, 0 to 100, 108 and calendar year, 1960 to 2009, for 12 countries of the Human Mortality Database (2015). Given 109 these data, we estimated observed mortality (or "observations") defined as deaths divided by 110 exposures by single years of age and calculated predicted mortality for each year separately with the 111 models of Gompertz, Makeham, and Siler. Henceforth the word "observations" means "occurrence- 112 exposure death rates." 113 2.1 Three theoretical models of mortality 114 We used mathematical expressions of the models of Gompertz, Makeham, and Siler that are based 115
- n the (old-age) modal age at death (Horiuchi et al. 2013; Missov et al. 2015; Bergeron-Boucher,
116 Ebeling, and Canudas-Romo 2015). The modal age at death is the age (beyond infancy and 117 childhood) at which the probability density of life table deaths has a maximum. The conventional 118 formulas for the models of Gompertz and Makeham use a parameter for an initial level of mortality 119 instead of the modal age at death. The formulas based on the modal age at death, given below, are 120 numerically more stable, have a better demographic interpretation, and are more comparable across 121 populations and points of time (Missov et al. 2015; Horiuchi et al. 2013). 122 The Gompertz model expresses mortality μ at age x in year t as 123 𝜈, = 𝛾𝑓(), 𝛾 > 0, 𝑁 > 0, for 𝑢 = 1, … , 𝑈, 𝑦 = 0, … , 𝑌. (1) 124 Here βt is the growth rate of mortality with age, Mt the modal age at death in year t, T the number of 125 years of observations, and X the maximum observed age. The Gompertz model predicts, on a 126 logarithmic scale of mortality and a linear scale of age, a linear increase in mortality from some 127 young age to the oldest age X = 100 here. 128
The Makeham model expresses mortality μ at age x in year t as 129 𝜈, = 𝑑 + 𝛾𝑓(), 𝑑 > 0. (2) 130 The parameter βt is the same as in the Gompertz model. Makeham added ct to represent background 131 mortality in year t, assumed to be the same at all ages x. The Makeham model predicts slowly 132 increasing mortality from infancy through childhood to young adulthood; thereafter, it models a 133 nearly linear increase in log mortality with increasing age. 134 The Siler model expresses mortality μ at age x in year t as 135 𝜈, = 𝛽𝑓, + 𝑑 + 𝛾,𝑓,(), 𝛽 > 0, 𝛾, > 0. (3) 136 Here 𝛾, = 𝛾 of the Makeham and Gompertz models. Siler adds two additional parameters: αt is 137 infant mortality, and β1,t is the rate of decline with increasing age x of childhood mortality in year t. 138 The Siler model predicts decreasing mortality from infancy to childhood, slowly increasing 139 mortality from childhood to young adulthood, and nearly linearly increasing log mortality with 140 increasing age throughout adulthood. 141 2.2 Taylor's law, mean and variance of mortality 142 TL describes a linear relationship of log10 of temporal variance (variance over time) to log10 of 143 temporal mean (mean over time) of mortality μ at age x: 144 𝑚𝑝𝑊𝑏𝑠(𝜈) = 𝑏 + 𝑐 ⋅ 𝑚𝑝𝐹(𝜈) (4) 145 where a is the intercept and b is the slope. With T years of observations or theoretical (fitted) values 146
- f mortality, the temporal mean of mortality μ at age x is
147 𝐹(𝜈) =
- ∑
𝜈,
- (5)
148 and the temporal variance is 149 𝑊𝑏𝑠(𝜈) =
- ∑
𝜈, − 𝐹(𝜈)
- .
(6) 150
We plot (on log-log coordinates) temporal variances and means of mortality for each age in one 151 national population at a time, separately for different national populations. These plots depict so- 152 called cross-age-scenarios of TL. 153 2.3 Statistical methods and visualization 154 2.3.1 Parameter estimation 155 We estimated the values of the parameters of the models of Gompertz, Makeham, and Siler from 156 deaths and exposures using the method of maximum likelihood. Specifically, we maximized a 157 Poisson log-likelihood in R (2015) with the function DEoptim (Mullen et al. 2011). 158 2.3.2 Analysis of log-log linearity 159 To analyze how closely TL approximates the log temporal mean and log temporal variance of 160
- bserved and/or modeled mortality, we used the linear correlation coefficient r2. The closer r2 is to
161
- ne, the better TL describes the relation of log temporal variance to log temporal mean of mortality.
162 2.3.3 Visualizing the age profile of TL 163 To compare the age profiles between observed and modeled mortality, we augmented the statistical 164 analysis and visualized the log10 temporal mean and log10 temporal variance of mortality by single- 165 year age groups using yellow and orange to represent children (0 to 20 years of age), red and 166 magenta for adults (21 to 60 years of age), and blue and green for older ages (61 to 100 years of 167 age). 168 2.3.4 Analysis of covariance 169 To analyze how well a theoretical model predicts the slope of TL fitted to observed mortality, we 170 used the analysis of covariance. 171
- 1. To determine whether the slopes of TL differ between observed and modeled mortality (by
172 sex, country, and model), we estimated a linear regression with an interaction term between the 173
variables log10E(μx) and a dichotomous variable model (with values "observed" and "model") using 174 the lm() function in R: 175 𝑚𝑝𝑊𝑏𝑠(𝜈) = 𝑑 + 𝑑𝑚𝑝𝐹(𝜈) + 𝑑𝑛𝑝𝑒𝑓𝑚 + 𝑑(𝑚𝑝𝐹(𝜈) × 𝑛𝑝𝑒𝑓𝑚). (7) 176 We use observed mortality as the reference level for the categorical variable model. The null 177 hypothesis was that 𝑑 = 0, i.e., that there was no difference between the model and the 178
- bservations in the slope of 𝑚𝑝𝑊𝑏𝑠(𝜈) as a linear function of 𝑚𝑝𝐹(𝜈). A very low p-value
179 indicated that the coefficient of the interaction term is non-zero, and that the slope of TL of a model 180 life table is not equal to the slope of TL of observed mortality data. 181
- 2a. We also used analysis of covariance to determine whether the slopes of TL differ between
182 males and females (by country and model). To analyze if the slopes of TL differed between 183 males and females, we estimated a linear regression with an interaction term between the variables 184 log10E(μx) and a dichotomous variable sex (with values "male" and "female"): 185 𝑚𝑝𝑊𝑏𝑠(𝜈) = 𝑒 + 𝑒𝑚𝑝𝐹(𝜈) + 𝑒𝑡𝑓𝑦 + 𝑒(𝑚𝑝𝐹(𝜈) × 𝑡𝑓𝑦). (8) 186 We used female mortality as the reference level. For the null hypothesis that 𝑒 = 0, a very low p- 187 value indicated that the coefficient 𝑒 of the interaction term is non-zero, and that the slope of TL is 188 different between males and females. 189
- 2b. To analyze if sex differences in the slope of TL differ between observed and modeled
190 mortality (by country and model), we estimated a linear regression with pairwise and three-way 191 interaction terms among the variables log10E(μx), sex, and model. Here, unlike equation (7) above, 192 the variable model had four values: 0 (observed), 1 (Gompertz), 2 (Makeham), 3 (Siler). Observed 193 mortality was the reference level for model, as in equation (7). For example, in testing the null 194 hypothesis that 𝑔
= 0, p = 0.00506 for the Gompertz model (model = 1) in relation to observed
195 mortality (model = 0) for all countries and p = 0.34987 for Siler (model = 3) in relation to observed 196 (model = 0) for all countries. We used female mortality as the reference level for sex. 197
𝑚𝑝𝑊𝑏𝑠(𝜈) = 𝑔
+ 𝑔 𝑚𝑝𝐹(𝜈) + 𝑔 𝑡𝑓𝑦 + 𝑔 𝑛𝑝𝑒𝑓𝑚
198 +𝑔
(𝑚𝑝𝐹(𝜈) × 𝑡𝑓𝑦) + 𝑔 (𝑚𝑝𝐹(𝜈) × 𝑛𝑝𝑒𝑓𝑚) + 𝑔 (𝑡𝑓𝑦 × 𝑛𝑝𝑒𝑓𝑚)
199 +𝑔
(𝑚𝑝𝐹(𝜈) × 𝑡𝑓𝑦 × 𝑛𝑝𝑒𝑓𝑚).
(9) 200 The null hypothesis is that 𝑔
= 0, i.e., that model has no influence on the interaction between sex
201 and 𝑚𝑝𝐹(𝜈). 202 2.4 Availability of data and supplementary information 203 In addition to the data on mortality, which are publicly available from the Human Mortality 204 Database (2015), supplementary information deposited with this paper includes a spreadsheet 205 (TLinMortalityModels.csv) with the values of 41 variables and a text file (TLinMortalityModels- 206 Documentation-Variables.txt) that defines these variables. The spreadsheet gives the parameter 207 estimates of the models of Gompertz, Makeham, and Siler for observed female and male mortality 208 from 1960 to 2009 in 12 countries of the Human Mortality Database (2015). This information is 209 graphed in figures 1-17 and supplementary figures A1-A20. 210
- 3. Results
211 3.1 Fitted mortality of Gompertz, Makeham, and Siler models 212 Before we analyze how consistent the models of Gompertz, Makeham, and Siler are with TL, we 213 first show how well they fit observed mortality. Figs. 1 and 2 display the observed age-specific 214 mortality (on a logarithmic scale) as a function of age from 0 to 100, for women and men, 215 respectively, from 1960 (light gray) to 2009 (black) in 12 countries of the Human Mortality 216 Database (2015). Fitted mortality is depicted in green, blue and red for the models of Gompertz, 217 Makeham, and Siler, respectively, in 2009 for each country. 218
- Figs. 1 and 2 here.
219
The observed mortality shows a typical age pattern: a fall from infancy to around age 10, an 220 "accident bump" around age 20 (often more pronounced for men than for women), and a roughly 221 linear rise on the log scale beyond age 30. Mortality at each age declined with time in many 222 developed countries since 1960. The declines occurred mainly at younger ages before they spread 223 towards higher ages (Christensen et al. 2009; Rau et al. 2008; Vaupel 2010). 224 The Gompertz model fitted observed mortality better at adult and older ages than at younger ages, 225 where the predicted mortality was systematically and substantially too low. The Makeham model 226 fitted better than the Gompertz model, particularly for younger ages, but the modeled mortality 227 increased monotonically with age, unlike the observations. The Siler model fitted the age profile of 228 mortality better than the Gompertz and Makeham models. None of the models reproduced the 229
- bserved "accident bump" of excess mortality of young adult ages. The findings in this paragraph
230 confirmed prior observations by others about the fit between human mortality data and the 231 Gompertz, Makeham, and Siler models (e.g., Bongaarts 2005; Canudas-Romo 2008; Horiuchi et al. 232 2013; Bergeron-Boucher, Ebeling, and Canudas-Romo 2015). 233 3.2 Statistical and visual tests of TL in observed and fitted mortality 234 This section reports the statistical analysis and visual tests proposed in section 2. Figs. 3 to 10 235 display the cross-age-scenarios of TL for observed and fitted mortality of women and men, 236 respectively, in 12 countries of the Human Mortality Database (2015). Odd-numbered figures are 237 for females, even-numbered for males. 238
- Figs. 3-10 here.
239 3.2.1 Log-log linearity and r2 values 240
- Figs. 1-2 compare the observed mortality with the three modeled mortality age schedules. Figs. 3-4
241 compare the temporal means and temporal variances of observed mortality with TL (the fitted least 242 squares straight line), on log-log coordinates. In these figures, r2 measures the linearity of observed 243
log temporal variance as a function of observed log temporal mean. In Figs. 5-10, r2 measures the 244 linearity of the log temporal variance of modeled mortality as a function of the log temporal mean 245
- f modeled mortality.
246 TL describes well the observed mortality (Figs. 3, 4) and the mortality of the models of Gompertz 247 (Figs. 5, 6), Makeham (Figs. 7, 8), and Siler (Figs. 9, 10). For observations on women, 0.96 ≤ r2 ≤ 248 0.99, and for men, 0.95 ≤ r2 ≤ 0.99 in the selected countries. Where the mortality models had r2 ≥ 249 0.999, sometimes there was excellent agreement with the strictly linear relationship posited by TL 250 (e.g., the Gompertz model for East Germany in Fig. 5 and the Makeham model for France and 251 Japan in Fig. 7). In some cases the models, and particularly the Gompertz model, predicted a 252 relation of log variance to log mean that was closer to linear than was the relation of log variance to 253 log mean based on observed mortality. The Gompertz model had r2 ≥ 0.99 more often than the other 254 two models. 255 According to the r2 values, TL describes Gompertz mortality best among these three models. 256 Appendix 1 gives a mathematical proof that TL describes Gompertz mortality exactly if the modal 257 age at death Mt increases linearly in time and if the rate of growth of mortality with age βt is 258 constant in time. The first assumption is close to reality, as we shall see. The second assumption is 259 not: βt increased slightly over time within a narrow range, even though βt is hypothesized to be 260 constant across individuals and over time (Vaupel 2010). Nevertheless, the excellent agreement 261 between TL and Gompertz mortality is at least partially explained by this mathematical analysis. 262 3.2.2 Visually comparing age profiles between observed and modeled mortality 263 In this section, we visually compare the age pattern of TL between observed and modeled mortality. 264 TL in observed mortality data (Figs. 3-4) has a typical pattern that is similar for women and men in 265 many populations. Both the log10 temporal variance and the log10 temporal mean of mortality 266 increase linearly from young adulthood (red) to the elderly (green), and they decrease from infancy 267
(yellow) to childhood (orange). The changes in the log10 temporal mean are expected from the 268 increasing mortality with age at older ages and the decreasing mortality with age from infancy to 269
- childhood. The corresponding linear changes in the log10 temporal variance were not known prior to
270 the work of Bohk, Rau and Cohen (2015). 271 TL of Gompertz mortality (Figs. 5-6) mirrors the pattern of TL of the observations well at adult 272 and old ages. However, both the log10 temporal variance and the log10 temporal mean of mortality 273
- f infants and children (yellow to orange) are modeled to be smaller than those of young adults
274 (red), unlike the observations. This major difference between observed mortality and the Gompertz 275 model arises because the Gompertz model assumes a log-linear increase in mortality from the 276 youngest to the oldest age. The Gompertz model captures neither declining mortality from infancy 277 to childhood nor its related effect on TL. 278 TL of Makeham mortality (Figs. 7-8) mirrors the pattern of TL of the observations well at adult 279 and old ages. However, both the log10 temporal variance and the log10 temporal mean of mortality 280 are modeled to be almost equal for infants and children (yellow to orange), on the one side, and 281 young adults (red), on the other side, unlike the observed mortality and Gompertz mortality. These 282 major differences arise because the Makeham model assumes that mortality increases slowly from 283 infancy to young adulthood and increases exponentially thereafter. As a consequence, the Makeham 284 model captures neither the decline in observed mortality from infancy to childhood nor its related 285 effect on TL. As expected, TL of Makeham mortality is closer than TL of Gompertz mortality to TL 286
- f observations.
287 TL of Siler mortality (Figs. 9-10) mirrors reasonably well the pattern of TL of the observations for 288 all ages in most of the 12 countries. The term in the Siler model that models declining mortality 289 from infancy to childhood captures the related effect on TL. 290 From visually comparing the age profiles, we conclude that the TL of the Siler model (fitted to 291
- bserved mortality) is closest to the TL of observed mortality.
292
3.2.3 Slopes of TL 293 In this section, we compare the slopes of TL between observed and modeled mortality. 294
- A. Visual overview
295
- Fig. 11 displays the slope of TL for women on the horizontal axis and the slope of TL for men on
296 the vertical axis for 12 countries of the Human Mortality Database (2015). Slopes are estimated 297 from observed mortality (black) and from the fitted models of Gompertz (green), Makeham (blue), 298 and Siler (red). Fig. 11 summarizes 96 slopes (96 = 12 × 4 × 2). Only two slopes exceeded 2 (for 299 TL fitted to the Gompertz model for Russian males, b = 2.02; and for TL fitted to the Siler model 300 for French females, b = 2.1). We regard these two slopes as outliers. All slopes exceeded 1. 301
- Fig. 11 here.
302 Slopes of TL estimated from observed mortality are closer to slopes estimated from the Makeham 303 model than they are to the slopes estimated from the other two models. Women and men have 304 greater slopes according to the Siler model than are estimated from observed mortality. Hence the 305 Siler model assumes more rapid increases in the variance of mortality with increasing mean 306 mortality than is observed. Women and men have substantially smaller slopes according to the 307 Gompertz model than are estimated from observed mortality. The Gompertz model assumes slower 308 increases in the variance of mortality with increasing mean mortality than is observed. 309 The diagonal line in Fig. 11 represents equal TL slopes for women and men. Sex differences in 310 slopes of TL are given in Fig. 11 by vertical deviations above or below the diagonal. Sex 311 differences appear to be slightly smaller for observed mortality and the Makeham model than for 312 the Gompertz and Siler models. Exceptional outliers are the slopes of TL of Gompertz mortality for 313 countries with relatively high mortality such as Russia, Hungary, and Poland (Grigoriev, 314 Doblhammer-Reiter, and Shkolnikov 2013; Grigoriev et al. 2010; Shkolnikov et al. 2013). 315
- B. Covariance analysis
316
We examine differences in the slopes of TL between sexes and models using covariance analysis. 317
- B1. Does the slope of TL for observed mortality differ from the slopes of TL for models?
318 The p-values of the test for the significance of the interaction term c3 in the analysis of covariance, 319
- eq. (7), are given by sex, country, and model (Gompertz, Makeham, Siler) in Table 1. This analysis
320 confirms the previous findings of Fig. 11. Specifically, the slope of TL of the Makeham model is 321 not significantly different from the slope of TL of observed mortality for women and men in almost 322 all of the 12 selected countries. By contrast, the slope of TL of the Siler model is significantly 323 different from the slope of TL of observed mortality for women and men in almost all 12 countries. 324 An exception is, for example, Poland. The slope of TL of the Gompertz model is significantly 325 different from the slope of TL of observed mortality for women and men in almost all 12 countries. 326
- B2a. Does the slope of TL differ between males and females for observed mortality and for
327 models? 328 The p-values of the test for the significance of the interaction term d3 in eq. (8) are given by country 329 for observed mortality and models in Table 2. 330 Slopes of TL fitted to observed mortality are not significantly different between males and females 331 in almost all 12 countries. With p = 0.001, West Germany is the only exception. However, the 332 slopes of TL differ between males and females almost as strongly in countries like France, the UK, 333 Japan, and Sweden. The vertical deviations from the diagonal in Fig. 11 are similar for these four 334 countries. 335 The slopes of TL of modeled mortality differ significantly between males and females for many 336
- countries. These sex differences are slightly more pronounced in the models of Gompertz and Siler
337 than in the Makeham model. This supports the previous finding of Fig. 11. 338 East Germany is the only country for which the slopes of TL of observed and modeled mortality do 339 not differ between males and females. All the points for this country are almost on the diagonal in 340
- Fig. 11. We do not know if this agreement of male and female slopes indicates a problem in the
341 mortality data or a statistical fluctuation or some special feature of East Germany. 342
- B2b. Do the sex differences in the slope of TL differ between observed mortality and models?
343 Table 3 lists the p-values of the test for the significance of the interaction term f7 between 344 log10E(μx), sex, and model of eq. (9). Consistent with the previous findings of Fig. 11 and Table 2, 345 the sex differences in the slope of TL do not differ much between the observed mortality and the 346 models of Gompertz, Makeham, and Siler. Specifically, the sex differences in the slope of TL are 347 not significantly different between observed mortality and the Makeham model in each of the 12 348
- countries. The sex differences in the slope of TL differ significantly between observed mortality
349 and the Gompertz model in only three countries: Hungary, Russia, and the USA; and, though less 350 significantly, in Sweden, Japan, West Germany, France and Denmark. The sex differences in the 351 slope of TL differ significantly between observed mortality and the Siler model in only two 352 countries: Sweden and the USA; and, though less significantly, in Russia, France and Denmark. 353 That the sex differences in the slope of TL are significant for Hungary, Russia and Japan could be 354 explained by the increasing sex gap in life expectancy at birth in those countries in the 1980s and 355
- 1990s. By contrast, other European countries experienced a decline in the female-male differences
356 in mortality (Oksuzyan et al. 2008). 357 3.3 Mathematical proof and theoretical explanations for TL in Gompertz mortality 358 In this section, we prove mathematically that the Gompertz model can explain the form of TL under 359 certain conditions. We investigate theoretically whether the Gompertz model can explain the 360
- bserved parameter values of TL.
361 3.3.1 Gompertz mortality predicts TL with slope 2 under certain conditions 362 We prove mathematically (in Appendix 1) that the Gompertz model eq. (1) with modal age at death 363 𝑁 increasing linearly in time and 𝛾 = 𝛾 > 0 obeys a cross-age-scenario of TL exactly with slope 364
b = 2. Appendix 1 gives an explicit form for the intercept of TL and a detailed proof. This theorem 365 gives analytically the exact relation between the parameters of the Gompertz model and the 366 parameters of TL in one simple case. 367 3.3.2 Temporal trend of 𝛾 alters the slope of TL fitted to Gompertz mortality 368 The theorem's assumptions that βt is constant over time and that the modal age at death Mt increases 369 linearly with time t cannot describe the reality of many countries since, empirically, the slope b of 370 TL fitted to the temporal mean and the temporal variance of observed mortality was always less 371 than 2 (Figs. 3-4), ranging from 1.65 to 1.87. 372 The numerical estimates of the parameters of all three mortality models, separately for females and 373 males, for all countries and years, along with the parameters of linear regressions of these 374 parameters as functions of time, are given in the Supplementary spreadsheet and graphed in 375 Supplementary Figs. A1-A20. 376 In the Gompertz model, even if the mode 𝑁 increases approximately linearly with time (as shown 377 in Figs. A3-A4), the coefficient 𝛾 must change in time so that, with increasing age, the variance of 378 mortality does not increase as fast as the square of the mean mortality. Empirically, the annual 379 estimates of 𝛾 increase approximately linearly over time for females (Fig. A1) and males (Fig. A2) 380 for all 12 countries. 381
- A. Theoretical analysis
382 We now analyze the impact of a temporal trend in 𝛾 on the estimated slope b of a cross-age- 383 scenario of TL fitted to Gompertz mortality rates. In the Gompertz model eq. (1), 𝛾 appears twice, 384 as a linear coefficient and in the exponent. We introduce separate notation for these two 385 appearances of 𝛾 so that we may analyze separately the two different effects of the temporal trend 386 in 𝛾: 387 𝜈, = 𝛾,𝑓,(). 388
We examine two cases. 389 Case 1 If 𝛾, is constant over time and 𝛾, changes linearly over time, then 𝜈, may be 390 factored into one factor 𝑓, that depends on age x only, not on time t, and another factor 391 𝛾,𝑓, that depends on time t only, and not on age x. In this case, the analysis used to 392 prove the theorem in Appendix 1 applies immediately (with slightly different expressions for the 393 intercept to allow for the temporal trend in 𝛾,). It follows from that analysis that TL describes 394 Gompertz mortality exactly with slope b = 2. Hence a temporal trend in 𝛾, cannot explain why 395 the empirical estimates of b are strictly less than 2. 396 Case 2 If 𝛾, changes linearly in time and 𝛾, is constant over time, then 𝛾, has no effect 397
- n the slope b of TL (though 𝛾, does affect the intercept a of TL) because 𝛾, simply
398 rescales the values of 𝜈,. If 𝛾, = 𝑡 + 𝑡𝑢 > 0, 𝑡 ≠ 0 and, as in the theorem, if 𝑁 = 𝑤 + 𝑥 ⋅ 399 𝑢 > 0, 𝑤 > 0, 𝑥 ≠ 0, for 𝑢 = 1, … , 𝑈, then 400 𝛾,(𝑦 − 𝑁) = (𝑡 + 𝑡𝑢)(𝑦 − {𝑤 + 𝑥 ⋅ 𝑢}) = 𝑦(𝑡 + 𝑡𝑢) − (𝑡 + 𝑡𝑢){𝑤 + 𝑥 ⋅ 𝑢} 401 ≡ 𝑦𝑔(𝑢) + (𝑢). 402 Here 𝑔(𝑢) ≡ 𝑡 + 𝑡𝑢 is linear in time t and (𝑢) ≡ (𝑡 + 𝑡𝑢){𝑤 + 𝑥 ⋅ 𝑢} is quadratic in time t. 403 Then 404 𝐹(𝜈) = 1 𝑈 𝜈,
- = 𝛾,
𝑈 exp𝑦𝑔(𝑢) + (𝑢)
- ,
405 𝑊𝑏𝑠(𝜈) = 1 𝑈 𝜈,
- − 𝐹(𝜈)
= 𝛾,
- 𝑈
exp 2𝑦𝑔(𝑢) + (𝑢)
- − 𝐹(𝜈)
.
406 In this case, we are not able to express log 𝑊𝑏𝑠(𝜈) explicitly as a function of log 𝐹(𝜈). 407
- B. Numerical experiment
408
Instead, we conducted a numerical experiment for women and men of 12 countries of the HMD. 409 This numerical experiment provides concrete answers conditional on the observed mortality, and 410 may guide possible future mathematical analysis. As an example, we describe our analysis of the 411
- bserved mortality for Denmark's females from 1960 to 2009.
412 Input data A Gompertz model fitted by maximum likelihood to each year's mortality as a function 413
- f age yielded time series of estimates of 𝛾 (Fig. A1) and of 𝑁 (Fig. A3) The supplementary
414 spreadsheet gives numerical values. These time series are summarized by the least-squares linear 415 approximations (shown to fewer significant digits in Figs. A1 and A3) 416 𝛾 = 0.085679264 + 0.00027542975 ⋅ 𝑢 , for 𝑢 = 1, … , 50, 417 𝑁 = 𝑤 + 𝑥 ⋅ 𝑢 = 80.97560676 + 0.098866512 ⋅ 𝑢 , for 𝑢 = 1, … , 50. 418 It seems helpful to appreciate the practical meaning of these two equations. The second equation 419 asserts that Danish females had modal age at death of approximately 81 years in 1960, and that 420 every year thereafter their modal age at death increased by just less than 0.1 year of age per 421 calendar year. According to this regression, in 2009, 50 years after 1960, Danish females had a 422 modal age of death of approximately 86 years (≈ 81 + 50 × 0.1). If the modal age at death increases, 423 why is the rate of increase of mortality with age, 𝛾, increasing (albeit very slowly)? In the 424 framework of the Gompertz model, the age that matters for mortality (the "effective age") is not the 425 chronological age x but the excess of the chronological age over the modal age at death, x - Mt. As 426 the modal age at death increases 0.1 year of age per calendar year, for each given chronological age 427 x, the effective age x - Mt gets younger by 0.1 year of age per calendar year. Deaths occur at 428 progressively later ages and (because of increasing 𝛾) mortality rises (slightly) more rapidly 429 (Canudas-Romo 2010; 2008). 430
Experimental design In a computational experiment, we put 𝑁 = 𝑤 + 𝑥 ⋅ 𝑢 as assumed above. 431 Then we calculated numerically three sets of values of 𝜈, for each age x = 0, ..., 100 and each year 432 t = 1, …, 50. In the first set of values, for the standard Gompertz model with 𝛾, = 𝛾, = 𝛾, 433 𝜈, = 𝛾𝑓(). 434 In the second set of values, for the Gompertz model with 𝛾, = 𝛾 and 𝛾, = 𝛾, 435 𝜈,
= 𝛾𝑓().
436 In the third set of values, for the Gompertz model with 𝛾, = 𝛾 and 𝛾, = 𝛾, 437 𝜈,
= 𝛾𝑓().
438 From each set of values, we calculated the corresponding mean and variance of mortality over time 439 for each age x. 440 Results Figs. 16 and 17 show the log temporal variance as a function of the log temporal mean for 441 these three hypothetical mortality schedules; in addition, Figs. 12 and 13 show the results if 442 𝛾, = 𝛾; Figs. 14 and 15 show the results if 𝛾, = 𝛾. The results are similar for both sexes 443 in the 12 HMD countries. As an example, we describe the results for Danish women. 444
- Figs. 12-17 here.
445 For the standard Gompertz model 𝜈, (blue solid line) of Danish women in Fig. 16, the relation of 446 log temporal variance to log temporal mean is close to linear (as predicted by TL) except for the 447 large values of the mean and variance of old-age mortality in the upper right corner of the graph. A 448 fitted TL (dark blue solid line, log10 variance = -2.35 + 1.60 log10 mean) approximates the 449 Gompertz log temporal variance and log temporal mean closely over most of their range. 450 When 𝛾, changes linearly over time and 𝜸𝒖,𝒆𝒑𝒙𝒐 is constant over time, 𝜈,
gives a variance-
451 mean relationship (red solid line) that approximates the Gompertz log variance and log mean 452
closely but is slightly concave (on log-log coordinates). The average slope of this curve, estimated 453 by 454 log
- / log
- ,
455 is 1.64, close to the slope b = 1.60 of the fitted TL. Thus the second case considered above gives an 456 approximate explanation of the form and slope of the fitted TL. 457 By contrast, when 𝜸𝒖,𝒗𝒒 is constant over time and 𝛾, changes linearly in time, the relationship 458
- f log variance of 𝜈,
to log mean of 𝜈, , calculated numerically (green solid line) from
459 𝜈,
, is visually indistinguishable from linear and has a numerically estimated slope
460 indistinguishable from 2 (to a precision of at least 5 decimal places). These results confirm 461 numerically the above mathematical analysis of Case 1. This case cannot explain the slope of the 462 TL fitted either to observed mortality or to Gompertz model mortality. 463 In conclusion, in this example, the linear trend in 𝑁 and the linear trend in 𝛾, in combination 464 explain qualitatively and quantitatively why TL for Gompertz modeled mortality has slope notably 465 less than 2, unlike the slope of exactly 2 that would be expected theoretically if 𝛾, were constant 466 (regardless of whether 𝛾, is constant or changing in time). 467
- 4. Conclusion
468 4.1 Summary 469 For females and males in 12 developed countries, the temporal means and temporal variances from 470 1960 to 2009 of observed age-specific mortality for each age from 0 to 100 years, when plotted on 471 log-log coordinates, were approximately linearly related, according to the data of the Human 472 Mortality Database (2015) (Bohk, Rau, and Cohen 2015). This approximate linearity was consistent 473 with Taylor's law. Here we sought to explain this pattern. 474
We compared TL fitted to temporal means and temporal variances of observed mortality with TL 475 fitted to mortality in the models of Gompertz (1825), Makeham (1860), and Siler (1979, 1983). 476 These models have progressively more parameters and, in the same order, fit the age profile of 477
- bserved mortality progressively more closely.
478 We analyzed how well each mortality model's TL matched TL fitted to observed mortality by 479 comparisons of three features: the log-log linearity of the means and variances of the modeled 480 mortality, the age profile (defined as the set of pairs of log(temporal mean mortality at age x) and 481 log(temporal variance of mortality at age x), for all ages x), and the slope. 482 For log-log linearity, we found that TL approximated mortality in the fitted models of Gompertz, 483 Makeham, and Siler more closely than TL approximated observed mortality. As a consequence, r2 484 values of TL of the Gompertz model were very close, and rounded, to 1. Compared to the Gompertz 485 model, the models of Makeham and Siler resulted in closer fits to observed mortality and to the TL 486
- f observed mortality. Consequently, the r2 values of TL of the models of Makeham and Siler were
487
- ften slightly smaller than those of Gompertz, but were also often closer to those of the observed
488 mortality. 489 For the age profile of TL, we found that the TL of the Siler model fitted to observed mortality had 490 an age profile that was closer to the age profile of TL of observed mortality than were the age 491 profiles of TL of the fitted models of Makeham and Gompertz. 492 For the slopes of TL, we found that the TL of the Makeham model fitted to observed mortality had 493 a slope that was closest to the slope of TL fitted directly to observed mortality, among the three 494
- models. Differences in the slope of TL between males and females in the fitted Makeham models
495 were also closest to the differences in the slope of TL between males and females of observed 496 mortality. 497
In addition to these empirical and statistical insights, we demonstrated mathematically that the log 498 temporal means and log temporal variances of mortality in the Gompertz model satisfy TL exactly 499 with slope b = 2 and an explicitly determined intercept when the modal age at death in the 500 Gompertz model increases linearly with time and the βt parameter for the increase of mortality with 501 age is constant in time t or 𝛾, is constant in time and 𝛾, changes linearly in time. As the 502 Gompertz model is a special case of the more complex models of Makeham and Siler, these 503 theoretical findings also apply to certain parameter values of the other two models. 504 Empirically, however, the slopes of TL fitted to observed mortality ranged from 1.65 to 1.87 and 505 the slopes of TL for the mortality models were all at least 1.28 and smaller than 2 (apart from the 506 two exceptions noted above, for Gompertz model mortality of Russian males and Siler model 507 mortality of French females). To explain why the slopes of TL fitted to observed mortality and the 508 fitted models were notably smaller than 2 (with the two exceptions just noted), our computational 509 experiments showed that, in the presence of an increasing modal age at death, it was necessary and 510 sufficient to take into account in the Gompertz model a linear trend in 𝛾,. When 𝛾, increased 511 linearly in time, the slope of TL based on Gompertz mortality was less than 2, and when 𝛾, was 512 constant, the slope of TL based on Gompertz mortality was numerically (and mathematically) 513 indistinguishable from 2. We tested numerically and confirmed this explanation for women and 514 men in 12 countries of the HMD. These numerical results indicate that, as long as 𝛾,, the growth 515 rate of mortality with age, increases linearly with time, TL fitted to mortality will have a slope that 516 is not equal to 2. 517 To conclude, our empirical, statistical, mathematical, and numerical findings confirm that the 518 temporal TL is a regular pattern with deep roots in widely recognized models of the age pattern and 519 temporal evolution of human mortality. 520 4.2 Future research 521
These results raise further theoretical and empirical questions. 522 Our mathematical analysis of the Gompertz model remains incomplete when both parameters (the 523 modal age at death and the growth rate of mortality with age) change in time. Our computational 524 experiment gave clear results about this case, but we have not proved these results mathematically. 525 Mathematical analysis is needed to reveal the necessary and sufficient conditions for TL fitted to 526 Gompertz mortality to have a slope less than 2 (not merely different from 2). 527 It would be desirable to complete the mathematical analysis of the Gompertz model and to extend it 528 to the Makeham, Siler, and other more complex models, e.g., those of Heligman and Pollard (1980) 529 and Thiele (1872), and piecewise constant mortality models of, e.g., Brouhns et al. (2002) and 530 Currie et al. (2009). These models may provide more precise approximations to empirical age- 531 profiles of mortality. However, their larger number of parameters and their greater mathematical 532 complexity make them more difficult to analyze mathematically and to understand. Since our goal 533 here was to understand an empirical pattern in a transparent way, we focused on simpler mortality 534 models. 535 Future research may extend the analysis to still more complex models. A potentially productive 536 approach to analyzing temporal trends and variations in mortality would be to construct a 537 generalized linear model (GLM) of all the observed mortality rates simultaneously, as in Brouhns et 538
- al. (2002), Currie et al. (2009), and Renshaw and Haberman (2006), and reviewed by Booth and
539 Tickle (2008). In a GLM approach, the dependent variable would be 𝜈, for all ages x, all years t, 540 both sexes, and all countries. The independent variables (predictors) would be age x, year t, sex 541 (female or male), country, and various higher-order (e.g., x2 and t2 to model curvature) and 542 interaction terms to be determined in the course of the analysis. The link function would be logit or 543 probit since 𝜈, is a fraction between 0 and 1. The coefficients of predictor t and t2 would quantify 544 the importance of systematic trends, linear and nonlinear, respectively. A GLM can estimate the 545 mean and the variance of 𝜈, simultaneously (for example, by using quasi-likelihood techniques for 546
the variance). With the estimates of means and variances of 𝜈, from a GLM, it would be possible 547 to test TL with finer resolution than has been possible with the traditional approach used here, in 548 which temporal means and temporal variances are computed independently for each age, sex, and 549 country. 550 A GLM could also be used to analyze mortality from each of our three models, and the structure 551 and coefficients of the GLM for modeled mortality could be compared with the structure and 552 coefficients of the GLM for observed mortality. This comparison would permit an evaluation of the 553 models with finer resolution than has been possible with the traditional approach used here. 554 Another empirical question and approach prompted by a reviewer's question is this. For any fixed 555 age x, observed mortality 𝜈, over the 50 years t=1960, …, 2009 may have a systematic trend, 556 fluctuations from this trend in each year t, and an interaction between the trend and the fluctuations 557 (e.g., temporal heteroscedasticity or temporal changes in the skewness of fluctuations). In future 558 research, it would be interesting to decompose the temporal mean and the temporal variance of 559
- bserved mortality at a given age into the contributions due to a systematic trend in time,
560 fluctuations, and their interaction; and to decompose the overall temporal TL of mortality into 561 components arising from trend, fluctuations, and interaction. A parallel theoretical analysis could 562 decompose age-specific mortality from models that explicitly incorporated stochastic fluctuations in 563 mortality, unlike the Gompertz, Makeham and Siler models. This empirical investigation could 564 provide a foundation for new theory generalizing the Gompertz and other models to allow for 565 stochastic fluctuations in mortality over time. 566 Reviewer Hal Caswell posed a more general theoretical question that is also related to variation in 567
- mortality. Temporal fluctuations in mortality rates are a component of a demographic model in a
568 stochastic environment. What are the consequences for stochastic population growth of greater 569 temporal variance in mortality at (older) ages where the mean mortality is also higher? This 570
question shows the potential use of TL applied to mortality in modeling and simulating stochastic 571 age-structured populations. 572 The above outlines of potential applications of TL in human mortality indicate TL's possible 573 usefulness and relevance in formal and empirical demographic research. 574
- 5. Acknowledgments
575 We thank three reviewers (including Hal Caswell, who identified himself) and the Associate Editor 576 Jakub Bijak for helpful comments and suggestions. [Remainder of acknowledgments to be restored 577 after blinding is removed.] 578 579
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Appendix 1. Taylor's law with slope 2 describes the Gompertz model 647
- Theorem. The Gompertz mortality model with modal age at death increasing linearly in time obeys
648 a cross-age-scenario of Taylor's law (TL) exactly with slope b = 2. Explicitly, assuming the 649 Gompertz model 𝜈, at age x and time t, 650 𝜈, = 𝛾𝑓(), 𝛾 > 0, 𝑁 > 0, for 𝑢 = 1, … , 𝑈, 𝑦 = 1, … , 𝑌, 651 with a linear change (increase or decrease) over time in the modal age at death 652 𝑁 = 𝑤 + 𝑥 ⋅ 𝑢 > 0, 𝑤 > 0, 𝑥 ≠ 0, for 𝑢 = 1, … , 𝑈, 653 and an exponential rate increase of mortality with age x that is constant over time t 654 𝛾 = 𝛾 > 0, for 𝑢 = 1, … , 𝑈, 655 then TL holds with slope 2 and intercept log(𝐿 − 𝐿
) − 2 log 𝐿 on log-log coordinates:
656 log 𝑊𝑏𝑠(𝜈) = log
- + 2 ⋅ log 𝐹(𝜈), for 𝑦 = 1, … , 𝑌,
657 where the positive constants 𝐿, 𝐿 are defined below. 658
- Proof. From the assumptions,
659 𝜈, = 𝛾𝑓() = 𝛾𝑓({⋅}) = 𝛾𝑓()𝑓 660 which implies that 𝜈, is an exponentially increasing function of age x for every time t. It also 661 implies that 𝜈, is an exponentially decreasing function of time t for every age x if w > 0, and is an 662 increasing function of time t for every age x if w < 0. Then, using the definitions in the main text of 663 𝐹(𝜈) as the temporal mean and 𝑊𝑏𝑠(𝜈) as the temporal variance of mortality at age x, 664 𝐹(𝜈) = 1 𝑈 𝜈,
- = 1
𝑈 𝛾𝑓() 𝑓
- = 𝑓 𝛾𝑓
𝑈 𝑓
- ,
665
where the first factor 𝑓 varies with age x only and the bracketed second factor varies with time t 666 and T only. Define 667 𝐿 ≡ 𝛾𝑓 𝑈 𝑓
- , 𝑟 ≡ 𝑓 .
668 𝐿 does not depend on age x. Then since 𝛾 > 0, 𝑥 ≠ 0, we have 𝑟 < 1 if w > 0 and q > 1 if w < 0 669 and in both cases 670 𝐿 = 𝛾𝑓 𝑈 (𝑟 + 𝑟 + ⋯ + 𝑟) = 𝛾𝑓 𝑈 𝑟(1 + 𝑟 + ⋯ + 𝑟) = 𝛾𝑓 𝑈 ⋅ 𝑟(1 − 𝑟) 1 − 𝑟 . 671 Since 𝐿 > 0, 𝐹(𝜈) = 𝐿𝑓 increases exponentially at rate β with increasing x. Also 672 𝑊𝑏𝑠(𝜈) = 1 𝑈 𝜈, − 𝐹(𝜈)
- = 1
𝑈 𝜈,
- − 𝐹(𝜈)
- 673
= 1 𝑈 𝛾𝑓()𝑓
- − 𝐿𝑓
= 𝑓 𝛾𝑓
𝑈 𝑓
- − 𝐿
𝑓.
674 Define 675 𝐿 ≡ 𝛾𝑓 𝑈 𝑓
- .
676 𝐿 does not depend on age x. Then 677 𝐿 = 𝛾𝑓 𝑈 (𝑟⋅ + 𝑟⋅ + ⋯ + 𝑟⋅) = 𝛾𝑓 𝑈 𝑟(1 − 𝑟⋅()) 1 − 𝑟 . 678 Also 679 𝑊𝑏𝑠(𝜈) = (𝐿 − 𝐿
)𝑓.
680 By Cauchy's inequality, 𝐿 − 𝐿
> 0. Therefore 𝑊𝑏𝑠(𝜈) increases exponentially at rate 2β with
681 increasing age x. Thus, we showed that 682
𝐹(𝜈) = 𝐿𝑓, 683 𝑊𝑏𝑠(𝜈) = (𝐿 − 𝐿
)𝑓 .
684 Therefore 685 𝑊𝑏𝑠(𝜈) =
- 𝐹(𝜈)
.
□ 686 Appendix 2. Taylor's law with slope less than 2 describes the model of Makeham 687 In the Makeham model, eq. (2), the additivity of expectations yields 688 𝐹(𝜈) = 𝐹(𝑑) + 𝐹𝛾𝑓() = 𝐹(𝑑) + 𝐹(𝜈). 689 The subscript M denotes the Makeham model and the subscript G denotes the Gompertz model. 690 Calculating the variance in the Makeham model requires specifying the relation between 𝑑 and 691 𝛾𝑓(). Based on the parameter estimates of the Makeham model in Figs. A5-A10, we 692 examine this empirically plausible special case: 693 𝑑 = 𝑑𝑓, 𝑑 > 0, 𝑒 > 0, 694 𝛾 = 𝛾 > 0, 695 𝑁 = 𝑤 + 𝑥 ⋅ 𝑢 > 0, 𝑤 > 0, 𝑥 > 0. 696 Thus 697 𝜈, = 𝑑𝑓 + 𝑓𝛾𝑓{⋅}. 698 On the right side, the first term depends only on t, not on x, and the second term factors into one 699 factor 𝑓 that depends on x only and another factor that depends on t only. By summing geometric 700 series as in Appendix 1, we can get explicit expressions for the constant 𝐷 (and 𝐿 is identical to 701 that constant in the Gompertz model) in the expression 702 𝐹(𝜈) = 𝐷 + 𝐿𝑓. 703
With increasing age x, 𝐹(𝜈) grows as the factor 𝑓. Also, 704 𝜈,
= 𝑑𝑓 + 𝑓𝛾𝑓{⋅} + 2𝑑𝑓𝛾𝑓{⋅} .
705 Therefore 706 𝐹𝜈,
= 𝐷 + 𝐿𝑓 + 𝐿𝑓,
707 𝐹
(𝜈) = 𝐷 + 𝐿 𝑓 + 2𝐷𝐿𝑓,
708 𝑊𝑏𝑠
(𝜈) = 𝐹𝜈, − 𝐹 (𝜈) = 𝐷 − 𝐷 + (𝐿 − 𝐿 )𝑓 + (𝐿 − 2𝐷𝐿)𝑓.
709 The same elementary methods used in Appendix 1 can determine 𝐿, 𝐿 explicitly. 710 From Figs. A7-A8, 𝛾 ≈ 0.1 for both females and males. Hence as x increases from 0 to 100, 𝑓 711 increases from 𝑓 = 1 to approximately 𝑓 ≈ 2.2 × 10. Hence the term of 𝑊𝑏𝑠
(𝜈) that
712 contains the factor 𝑓, which is approximately 𝑓 ≈ 4.8 × 10 when x = 100, increasingly 713 dominates the term of 𝑊𝑏𝑠
(𝜈) that contains the factor 𝑓. So, to a first approximation,
714 neglecting all but the dominant terms, 𝑊𝑏𝑠
(𝜈) scales with increasing age x as the square of
715 𝐹(𝜈). Thus, asymptotically for increasing age x, TL holds approximately with slope 𝑐 ≈ 2. 716 This is only a first approximation. 𝐹(𝜈) and 𝑊𝑏𝑠
(𝜈) each contains a constant term, and
717 𝑊𝑏𝑠
(𝜈) contains a term with factor 𝑓 which scales more slowly than the dominant term of
718 𝑊𝑏𝑠
(𝜈) which contains the square of 𝑓. Thus 𝑊𝑏𝑠 (𝜈) scales with increasing x more slowly
719 than the square of 𝐹(𝜈), i.e., TL is expected to hold approximately with a slope less than 2. In all 720 12 countries, the estimated values of the TL slope never exceeded the Japanese record of b = 1.86 721 for females (Fig. 7) and never exceeded the Japanese and French records of b = 1.82 for males (Fig. 722 8). Both record values were substantially less than 2. Thus, we have given, in this special case, an 723 argument to explain why TL with slope less than 2 approximates the mortality of the Makeham 724 model reasonably well. 725
Tables 726
Table 1 727 Equal to TL of
- bserved data?
Gompertz Makeham Siler Women Men Both Women Men Both Women Men Both All countries 0.073200 0.284200 0.032000 0 Denmark 0.005358 0 0.022461 0.231000 0.284805 0.000312 0.208000 0.000392 France 0.748900 0.076500 0.486783 0 East Germany 0.000006 0 0.000580 0.329880 0.011300 0 0.000120 0 West Germany 0.351730 0.986726 0.432000 0 0.000014 0 Hungary 0.000007 0.001720 0.005730 0.296356 0.078070 0.106000 0.000661 0.008880 0.000077 Italy 0.003660 0.000132 0.000004 0.000001 0.001448 0 Japan 0.035169 0.001420 0.001870 0 Poland 0.032000 0 0.021900 0.811000 0.141000 0.233800 0.177000 0.153 Russia 0.009401 0 0.789410 0.000337 0.028860 0.002170 0.213779 0.000048 0.01896
Sweden 0.000002 0.532277 0.001853 0 0.000214 0 UK 0.002140 0.009960 0.000722 0.000380 0.000650 0.000003 USA 0.051616 0.114000 0.970258 0.000395 0 728 Table 1: P-values to test the null hypothesis of no differences in TL slope between observed data and the fitted models of Gompertz, Makeham, 729 and Siler, for women and men in 12 countries of the Human Mortality Database (2015). A p-value below 0.001 indicates that the coefficient of 730 the interaction term is statistically significantly non-zero. An entry of 0 means that the rounded value of p is 0.000000. 731
Table 2 732 733 Sex differences in TL? Observed data Gompertz Makeham Siler All countries 0.023190 0.087000 0.199000 0.000290 Denmark 0.644000 0.000844 0.000736 France 0.031800 0.204590 0.069400 0.000017 East Germany 0.306800 0.187000 0.943370 0.510000 West Germany 0.000968 0.336000 0.000136 Hungary 0.426000 0.920000 0.106000 Italy 0.126570 0.582600 0.000200 0.000514
Japan 0.003760 0.068200 0.000128 Poland 0.827000 0.000021 0.068100 0.335000 Russia 0.936100 0.095200 0.000035 Sweden 0.005600 UK 0.042600 0.000009 USA 0.171000 0.001040 0.001610 734 Table 2: P-values to test the null hypothesis of no differences between 735 females and males in the slope of TL fitted to observed death rates and 736 in the slope of TL fitted to the models of Gompertz, Makeham, and 737 Siler, in 12 countries of the Human Mortality Database (2015). A p- 738 value below 0.001 indicates that the coefficient of the interaction term 739 is statistically significantly non-zero. An entry of 0 means that the 740 rounded value of p is 0.000000. 741 742
Table 3 743 744 Sex differences in TL equal to
- bserved data?
Gompertz Makeham Siler All countries 0.005060 0.581010 0.349870 Denmark 0.025680 0.011860 0.045340 France 0.008070 0.164250 0.056650 East Germany 0.447548 0.392768 0.586554 West Germany 0.003030 0.527880 0.237640 Hungary 0.648766 0.515661 Italy 0.226781 0.329177 0.414148 Japan 0.029082 0.165447 0.817667
Poland 0.00917 0.128900 0.650510 Russia 0.303197 0.046573 Sweden 0.004344 0.006243 0.000250 UK 0.401217 0.643469 0.354857 USA 0.000003 0.013959 0.000247 745 Table 3: P-values to test the null hypothesis of no differences in the 746 sex differences in TL slope between observed mortality rates and 747 fitted models of Gompertz, Makeham, and Siler, in 12 countries of the 748 Human Mortality Database (2015). A p-value below 0.001 indicates 749 that the coefficient of the interaction term is non-zero. An entry of 0 750 means that the rounded value of p is 0.000000. 751 752
Figure captions 753
- 1. Observed female mortality from 1960 (light gray) to 2009
754 (black), and fitted female mortality with models of Siler (red), 755 Gompertz (green) and Makeham (blue) in 2009 for 12 756 countries of the Human Mortality Database (2015) 757
- 2. Observed male mortality from 1960 (light gray) to 2009
758 (black), and fitted male mortality with models of Siler (red), 759 Gompertz (green) and Makeham (blue) in 2009 for 12 760 countries of the Human Mortality Database (2015) 761
- 3. TL in observed female mortality for the ages 0 (yellow) to 100
762 (green) from 1960 1 to 2009 on a logarithmic scale (base=10) 763 for 12 countries of the Human Mortality Database (2015) 764
- 4. TL in observed male mortality for the ages 0 (yellow) to 100
765 (green) from 1960 to 2009 on a logarithmic scale (base=10) for 766 12 countries of the Human Mortality Database (2015) 767
- 5. TL in fitted female mortality of the Gompertz model for the
768 ages 0 (yellow) to 100 (green) from 1960 to 2009 on a 769
logarithmic scale (base=10) for 12 countries of the Human 770 Mortality Database (2015) 771
- 6. TL in fitted male mortality of the Gompertz model for the ages
772 0 (yellow) to 100 (green) from 1960 to 2009 on a logarithmic 773 scale (base=10) for 12 countries of the Human Mortality 774 Database (2015) 775
- 7. TL in fitted female mortality of the model of Makeham for the
776 ages 0 (yellow) to 100 (green) from 1960 to 2009 on a 777 logarithmic scale (base=10) for 12 countries of the Human 778 Mortality Database (2015) 779
- 8. TL in fitted male mortality of the model of Makeham for the
780 ages 0 (yellow) to 100 (green) from 1960 to 2009 on a 781 logarithmic scale (base=10) for 12 countries of the Human 782 Mortality Database (2015) 783
- 9. TL in fitted female mortality of the model of Siler for the ages
784 0 (yellow) to 100 (green) from 1960 to 2009 on a logarithmic 785 scale (base=10) for 12 countries of the Human Mortality 786 Database (2015) 787
- 10. TL in fitted male mortality of the model of Siler for the ages 0
788 (yellow) to 100 (green) from 1960 to 2009 on a logarithmic 789 scale (base=10) for 12 countries of the Human Mortality 790 Database (2015) 791
- 11. Scatterplot of slope of TL for women (horizontal axis) and
792 men (vertical axis) for 12 countries of the Human Mortality 793 Database (2015). Observations are in black, fitted data of the 794 models of Gompertz, Makeham, and Siler are depicted in red, 795 green, blue, and red, respectively. 796
- 12. TL (solid black line) in fitted female mortality of the model of
797 Gompertz with βt,up = constant for the ages 0 (yellow) to 100 798 (green) from 1960 to 2009 on a logarithmic scale (base=10) for 799 12 countries of the Human Mortality Database (2015) 800
- 13. TL (solid black line) in fitted male mortality of the model of
801 Gompertz with βt,up = constant for the ages 0 (yellow) to 100 802 (green) from 1960 to 2009 on a logarithmic scale (base=10) for 803 12 countries of the Human Mortality Database (2015) 804
- 14. TL (solid black line) in fitted female mortality of the model of
805 Gompertz with βt,down = constant for the ages 0 (yellow) to 100 806 (green) from 1960 to 2009 on a logarithmic scale (base=10) for 807 12 countries of the Human Mortality Database (2015) 808
- 15. TL (solid black line) in fitted male mortality of the model of
809 Gompertz with βt,down = constant for the ages 0 (yellow) to 100 810 (green) from 1960 to 2009 on a logarithmic scale (base=10) for 811 12 countries of the Human Mortality Database (2015) 812
- 16. TL (solid dark blue line) in fitted female mortality of the
813 model of Gompertz (solid blue line), of the model of Gompertz 814 with βt,up = constant (solid green line) and of the model of 815 Gompertz with βt,down = constant (solid red line) for the ages 0 816 to 100 from 1960 to 2009 on a logarithmic scale (base=10) for 817 12 countries of the Human Mortality Database (2015) 818
- 17. TL (solid dark blue line) in fitted male mortality of the model
819
- f Gompertz (solid blue line), of the model of Gompertz with
820 βt,up = constant (solid green line) and of the model of Gompertz 821 with βt,down = constant (solid red line) for the ages 0 to 100 822
from 1960 to 2009 on a logarithmic scale (base=10) for 12 823 countries of the Human Mortality Database (2015) 824
❋✐❣✉r❡ ✶✿ ❖❜s❡r✈❡❞ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢r♦♠ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛♥❞ ✜tt❡❞ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ✇✐t❤ ♠♦❞❡❧s ♦❢ ●♦♠♣❡rt③ ✭❣r❡❡♥✮✱ ▼❛❦❡❤❛♠ ✭❜❧✉❡✮✱ ❛♥❞ ❙✐❧❡r ✭r❡❞✮ ✐♥ ✷✵✵✾ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
Denmark
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
France
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
East Germany
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
West Germany
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Hungary
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Italy
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Japan
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Poland
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Russia
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Sweden
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
United Kingdom
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
USA
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Women Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
✶
❋✐❣✉r❡ ✷✿ ❖❜s❡r✈❡❞ ♠❛❧❡ ♠♦rt❛❧✐t② ❢r♦♠ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛♥❞ ✜tt❡❞ ♠❛❧❡ ♠♦rt❛❧✐t② ✇✐t❤ ♠♦❞❡❧s ♦❢ ●♦♠♣❡rt③ ✭❣r❡❡♥✮✱ ▼❛❦❡❤❛♠ ✭❜❧✉❡✮✱ ❛♥❞ ❙✐❧❡r ✭r❡❞✮ ✐♥ ✷✵✵✾ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
Denmark
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
France
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
East Germany
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
West Germany
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Hungary
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Italy
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Japan
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Poland
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Russia
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
Sweden
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
United Kingdom
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
USA
Age 20 40 60 80 100 1e−05 1e−04 0.001 0.01 0.1 1
Men Observed, 1960−2009 Gompertz, 2009 Makeham, 2009 Siler, 2009
✷
❋✐❣✉r❡ ✸✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ♦❜s❡r✈❡❞ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.94 + 1.7 * log E r2 = 0.975799
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.44 + 1.86 * log E r2 = 0.984697
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.42 + 1.84 * log E r2 = 0.990213
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.58 + 1.77 * log E r2 = 0.988214
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.97 + 1.75 * log E r2 = 0.964304
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.52 + 1.76 * log E r2 = 0.986376
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.1 + 1.82 * log E r2 = 0.993438
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.09 + 1.71 * log E r2 = 0.963367
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.22 + 1.74 * log E r2 = 0.9639
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.77 + 1.73 * log E r2 = 0.984705
- Age 0
Age 100
- ●
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.85 + 1.77 * log E r2 = 0.985661
- Age 0
Age 100
- ●
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.02 + 1.75 * log E r2 = 0.98053
- Age 0
Age 100
✸
❋✐❣✉r❡ ✹✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ♦❜s❡r✈❡❞ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.07 + 1.68 * log E r2 = 0.964255
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.71 + 1.78 * log E r2 = 0.977494
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.68 + 1.81 * log E r2 = 0.971128
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.83 + 1.67 * log E r2 = 0.983024
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.89 + 1.71 * log E r2 = 0.964113
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.74 + 1.71 * log E r2 = 0.979539
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.43 + 1.75 * log E r2 = 0.989407
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.17 + 1.72 * log E r2 = 0.959724
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.98 + 1.74 * log E r2 = 0.947776
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.99 + 1.65 * log E r2 = 0.985561
- Age 0
Age 100
- ●
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.65 + 1.87 * log E r2 = 0.955167
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.09 + 1.69 * log E r2 = 0.955195
- Age 0
Age 100
✹
❋✐❣✉r❡ ✺✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ●♦♠♣❡rt③ ♠♦❞❡❧ ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.35 + 1.6 * log E r2 = 0.996836
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.88 + 1.56 * log E r2 = 0.995251
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.65 + 1.66 * log E r2 = 0.999866
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.04 + 1.5 * log E r2 = 0.993258
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.41 + 1.54 * log E r2 = 0.99832
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.05 + 1.41 * log E r2 = 0.992195
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.66 + 1.51 * log E r2 = 0.996571
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.28 + 1.39 * log E r2 = 0.96932
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.29 + 1.62 * log E r2 = 0.928336
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.96 + 1.64 * log E r2 = 0.996364
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.2 + 1.55 * log E r2 = 0.993925
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.91 + 1.28 * log E r2 = 0.973313
- Age 0
Age 100
✺
❋✐❣✉r❡ ✻✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ●♦♠♣❡rt③ ♠♦❞❡❧ ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.62 + 1.48 * log E r2 = 0.995067
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.99 + 1.58 * log E r2 = 0.997221
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.81 + 1.65 * log E r2 = 0.998425
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.05 + 1.49 * log E r2 = 0.997557
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.14 + 1.86 * log E r2 = 0.995649
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.14 + 1.4 * log E r2 = 0.992906
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.15 + 1.38 * log E r2 = 0.991166
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.09 + 1.59 * log E r2 = 0.941446
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.54 + 2.02 * log E r2 = 0.994449
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.42 + 1.48 * log E r2 = 0.986869
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.89 + 1.61 * log E r2 = 0.998911
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.43 + 1.42 * log E r2 = 0.992291
- Age 0
Age 100
✻
❋✐❣✉r❡ ✼✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ▼❛❦❡❤❛♠ ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.8 + 1.79 * log E r2 = 0.959798
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.3 + 1.85 * log E r2 = 0.999997
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.4 + 1.77 * log E r2 = 0.990884
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.43 + 1.75 * log E r2 = 0.995328
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.82 + 1.8 * log E r2 = 0.93324
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.43 + 1.69 * log E r2 = 0.992601
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −0.94 + 1.86 * log E r2 = 0.999902
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.05 + 1.61 * log E r2 = 0.952084
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.8 + 1.57 * log E r2 = 0.987862
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.51 + 1.83 * log E r2 = 0.998736
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.79 + 1.71 * log E r2 = 0.99396
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.94 + 1.69 * log E r2 = 0.992182
- Age 0
Age 100
✼
❋✐❣✉r❡ ✽✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ▼❛❦❡❤❛♠ ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.19 + 1.65 * log E r2 = 0.981329
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.47 + 1.82 * log E r2 = 0.994978
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.61 + 1.77 * log E r2 = 0.96982
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.66 + 1.67 * log E r2 = 0.990423
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.82 + 1.79 * log E r2 = 0.940913
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.74 + 1.61 * log E r2 = 0.98951
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.16 + 1.82 * log E r2 = 0.991112
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.03 + 1.74 * log E r2 = 0.901258
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.27 + 1.64 * log E r2 = 0.941351
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.94 + 1.66 * log E r2 = 0.999324
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.55 + 1.78 * log E r2 = 0.999242
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.78 + 1.74 * log E r2 = 0.999927
- Age 0
Age 100
✽
❋✐❣✉r❡ ✾✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ❙✐❧❡r ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.79 + 1.84 * log E r2 = 0.974989
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −0.99 + 2.1 * log E r2 = 0.980245
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.22 + 1.95 * log E r2 = 0.996598
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.3 + 1.9 * log E r2 = 0.99691
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.78 + 1.91 * log E r2 = 0.966305
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.26 + 1.87 * log E r2 = 0.994721
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −0.88 + 1.92 * log E r2 = 0.99624
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.98 + 1.76 * log E r2 = 0.986279
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.59 + 1.68 * log E r2 = 0.989448
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.41 + 1.92 * log E r2 = 0.997769
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.64 + 1.85 * log E r2 = 0.997586
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.8 + 1.84 * log E r2 = 0.995283
- Age 0
Age 100
✾
❋✐❣✉r❡ ✶✵✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ❙✐❧❡r ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.15 + 1.72 * log E r2 = 0.991068
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.36 + 1.95 * log E r2 = 0.994916
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.47 + 1.94 * log E r2 = 0.988184
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.6 + 1.77 * log E r2 = 0.99632
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.88 + 1.83 * log E r2 = 0.96839
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.61 + 1.79 * log E r2 = 0.991095
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.17 + 1.86 * log E r2 = 0.996672
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.14 + 1.8 * log E r2 = 0.953993
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.38 + 1.56 * log E r2 = 0.978117
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.9 + 1.73 * log E r2 = 0.995576
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.34 + 1.98 * log E r2 = 0.991534
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.58 + 1.94 * log E r2 = 0.978225
- Age 0
Age 100
✶✵
❋✐❣✉r❡ ✶✶✿ ❙❝❛tt❡r♣❧♦t ♦❢ s❧♦♣❡ ♦❢ ❚▲ ❢♦r ✇♦♠❡♥ ✭❤♦r✐③♦♥t❛❧ ❛①✐s✮ ❛♥❞ ♠❡♥ ✭✈❡rt✐❝❛❧ ❛①✐s✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮✳ ❖❜s❡r✈❛t✐♦♥s ❛r❡ ✐♥ ❜❧❛❝❦✱ ✜tt❡❞ ❞❛t❛ ♦❢ t❤❡ ♠♦❞❡❧s ♦❢ ●♦♠♣❡rt③✱ ▼❛❦❡❤❛♠✱ ❛♥❞ ❙✐❧❡r ❛r❡ ❞❡♣✐❝t❡❞ ✐♥ ❣r❡❡♥✱ ❜❧✉❡✱ ❛♥❞ r❡❞✱ r❡s♣❡❝t✐✈❡❧②✳
TL, slope, women TL, slope, men 1.2 1.3 1.4 1.5 1.6 1.7 1.8 1.9 2.0 2.1 1.2 1.3 1.4 1.5 1.6 1.7 1.8 1.9 2.0 2.1 DNK DNK DNK DNK FRA FRA FRA FRA GDR GDR GDR GDR FRG FRG FRG FRG HUN HUN HUN HUN ITA ITA ITA ITA JPN JPN JPN JPN POL POL POL POL RUS RUS RUS RUS SWE SWE SWE SWE GBR GBR GBR GBR USA USA USA USA
- Observed
Gompertz Makeham Siler
✶✶
❋✐❣✉r❡ ✶✷✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✇✐t❤ βt,up = ❝♦♥st❛♥t ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.96 + 2 * log E r2 = 1
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.41 + 2 * log E r2 = 1
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.36 + 2 * log E r2 = 1
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.52 + 2 * log E r2 = 1
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.07 + 2 * log E r2 = 1
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.59 + 2 * log E r2 = 1
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.08 + 2 * log E r2 = 1
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.98 + 2 * log E r2 = 1
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.71 + 2 * log E r2 = 1
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.6 + 2 * log E r2 = 1
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.74 + 2 * log E r2 = 1
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.2 + 2 * log E r2 = 1
- Age 0
Age 100
✶✷
❋✐❣✉r❡ ✶✸✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✇✐t❤ βt,up = ❝♦♥st❛♥t ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.21 + 2 * log E r2 = 1
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.49 + 2 * log E r2 = 1
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.5 + 2 * log E r2 = 1
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.51 + 2 * log E r2 = 1
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.03 + 2 * log E r2 = 1
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.69 + 2 * log E r2 = 1
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.35 + 2 * log E r2 = 1
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.8 + 2 * log E r2 = 1
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.54 + 2 * log E r2 = 1
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.87 + 2 * log E r2 = 1
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.45 + 2 * log E r2 = 1
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.69 + 2 * log E r2 = 1
- Age 0
Age 100
✶✸
❋✐❣✉r❡ ✶✹✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✇✐t❤ βt,down = ❝♦♥st❛♥t ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.02 + 1.67 * log E r2 = 0.998115
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.5 + 1.64 * log E r2 = 0.997767
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.48 + 1.67 * log E r2 = 0.999758
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.61 + 1.58 * log E r2 = 0.996207
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.21 + 1.55 * log E r2 = 0.998019
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.65 + 1.47 * log E r2 = 0.990452
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.27 + 1.57 * log E r2 = 0.997608
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.36 + 1.24 * log E r2 = 0.988124
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.71 + 1.35 * log E r2 = 0.945995
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.63 + 1.7 * log E r2 = 0.998369
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.8 + 1.64 * log E r2 = 0.997375
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.28 + 1.42 * log E r2 = 0.984253
- Age 0
Age 100
✶✹
❋✐❣✉r❡ ✶✺✿ ❚▲ ✭s♦❧✐❞ ❜❧❛❝❦ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✇✐t❤ βt,down = ❝♦♥st❛♥t ❢♦r t❤❡ ❛❣❡s ✵ ✭②❡❧❧♦✇✮ t♦ ✶✵✵ ✭❣r❡❡♥✮ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.31 + 1.53 * log E r2 = 0.994336
- Age 0
Age 100
- France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.67 + 1.65 * log E r2 = 0.998622
- Age 0
Age 100
- East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.74 + 1.61 * log E r2 = 0.999726
- Age 0
Age 100
- West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.74 + 1.53 * log E r2 = 0.996885
- Age 0
Age 100
- Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.26 + 1.75 * log E r2 = 0.997664
- Age 0
Age 100
- Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.89 + 1.4 * log E r2 = 0.991416
- Age 0
Age 100
- Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.65 + 1.49 * log E r2 = 0.994626
- Age 0
Age 100
- Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −2.49 + 1.28 * log E r2 = 0.964275
- Age 0
Age 100
- Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.83 + 1.82 * log E r2 = 0.991599
- Age 0
Age 100
- Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.93 + 1.6 * log E r2 = 0.994367
- Age 0
Age 100
- United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.63 + 1.66 * log E r2 = 0.998985
- Age 0
Age 100
- USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 log Var = −1.95 + 1.53 * log E r2 = 0.996026
- Age 0
Age 100
✶✺
❋✐❣✉r❡ ✶✻✿ ❚▲ ✭s♦❧✐❞ ❞❛r❦❜❧✉❡ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✭s♦❧✐❞ ❜❧✉❡ ❧✐♥❡✮✱ ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✇✐t❤ βt,up = ❝♦♥st❛♥t ✭s♦❧✐❞ ❣r❡❡♥ ❧✐♥❡✮ ❛♥❞ ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✇✐t❤ βt,down = ❝♦♥st❛♥t ✭s♦❧✐❞ r❡❞ ❧✐♥❡✮ ❢♦r t❤❡ ❛❣❡s ✵ t♦ ✶✵✵ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
✶✻
❋✐❣✉r❡ ✶✼✿ ❚▲ ✭s♦❧✐❞ ❞❛r❦❜❧✉❡ ❧✐♥❡✮ ✐♥ ✜tt❡❞ ♠❛❧❡ ♠♦rt❛❧✐t② ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✭s♦❧✐❞ ❜❧✉❡ ❧✐♥❡✮✱ ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✇✐t❤ βt,up = ❝♦♥st❛♥t ✭s♦❧✐❞ ❣r❡❡♥ ❧✐♥❡✮ ❛♥❞ ♦❢ t❤❡ ♠♦❞❡❧ ♦❢ ●♦♠♣❡rt③ ✇✐t❤ βt,down = ❝♦♥st❛♥t ✭s♦❧✐❞ r❡❞ ❧✐♥❡✮ ❢♦r t❤❡ ❛❣❡s ✵ t♦ ✶✵✵ ❢r♦♠ ✶✾✻✵ t♦ ✷✵✵✾ ♦♥ ❛ ❧♦❣❛r✐t❤♠✐❝ s❝❛❧❡ ✭❜❛s❡❂✶✵✮ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
Denmark
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
France
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
East Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
West Germany
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Hungary
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Italy
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Japan
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Poland
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Russia
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
Sweden
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
United Kingdom
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
USA
E(m) Var(m) 1e−04 0.001 0.01 0.1 1 1e−08 1e−06 1e−04 0.01 Gompertz Gompertz, TL βt,up = constant βt,down = constant
✶✼
❋✐❣✉r❡ ❆✶✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r β ♦❢ t❤❡ ●♦♠♣❡rt③ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.08568 + 0.00028 * t r2 = 0.878622
- France
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.08147 + 0.00053 * t r2 = 0.964409
- East Germany
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.08804 + 0.00049 * t r2 = 0.892376
- West Germany
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.08313 + 0.00062 * t r2 = 0.969091
- Hungary
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.07927 + 0.00034 * t r2 = 0.906444
- Italy
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.07303 + 0.00092 * t r2 = 0.94199
- Japan
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.07752 + 0.00074 * t r2 = 0.888995
- Poland
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.0651 + 0.00079 * t r2 = 0.917214
- Russia
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.06996 + 0.00038 * t r2 = 0.670455
- Sweden
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.09242 + 4e−04 * t r2 = 0.966379
- United Kingdom
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.08361 + 4e−04 * t r2 = 0.971975
- USA
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.07025 + 0.00047 * t r2 = 0.972012
✶
❋✐❣✉r❡ ❆✷✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r β ♦❢ t❤❡ ●♦♠♣❡rt③ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.0764 + 0.00035 * t r2 = 0.96477
- France
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.06995 + 0.00034 * t r2 = 0.96677
- East Germany
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.07513 + 0.00034 * t r2 = 0.737719
- West Germany
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.07137 + 0.00054 * t r2 = 0.95665
- Hungary
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.07016 + 0.00014 * t r2 = 0.57982
- Italy
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.06366 + 0.00076 * t r2 = 0.957143
- Japan
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.07086 + 0.00058 * t r2 = 0.892024
- Poland
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.05679 + 0.00052 * t r2 = 0.84183
- Russia
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.057 + 0.00015 * t r2 = 0.369078
- Sweden
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.0806 + 0.00045 * t r2 = 0.950942
- United Kingdom
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.07784 + 0.00036 * t r2 = 0.934544
- USA
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.06432 + 0.00035 * t r2 = 0.937372
✷
❋✐❣✉r❡ ❆✸✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r M ♦❢ t❤❡ ●♦♠♣❡rt③ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 80.97561 + 0.09887 * t r2 = 0.90672
- France
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 80.08741 + 0.19684 * t r2 = 0.990619
- East Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 77.59136 + 0.18311 * t r2 = 0.888607
- West Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 78.87917 + 0.17929 * t r2 = 0.986818
- Hungary
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 78.03761 + 0.09608 * t r2 = 0.807261
- Italy
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 79.32194 + 0.202 * t r2 = 0.990541
- Japan
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 78.44894 + 0.27832 * t r2 = 0.991375
- Poland
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 79.62882 + 0.09399 * t r2 = 0.767071
- Russia
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 81.67332 + −0.04447 * t r2 = 0.496914
- Sweden
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 81.43884 + 0.13778 * t r2 = 0.981885
- United Kingdom
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 79.77629 + 0.14245 * t r2 = 0.985483
- USA
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 80.97135 + 0.12256 * t r2 = 0.915122
✸
❋✐❣✉r❡ ❆✹✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r M ♦❢ t❤❡ ●♦♠♣❡rt③ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 76.21324 + 0.09929 * t r2 = 0.829179
- France
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 73.13188 + 0.21 * t r2 = 0.979725
- East Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 72.59867 + 0.17007 * t r2 = 0.830681
- West Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 72.68379 + 0.20738 * t r2 = 0.970011
- Hungary
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 73.83969 + 0.00576 * t r2 = 0.004275
- Italy
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 73.7067 + 0.21092 * t r2 = 0.97651
- Japan
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 74.24889 + 0.23728 * t r2 = 0.975253
- Poland
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 73.89338 + 0.05044 * t r2 = 0.300505
- Russia
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 73.37373 + −0.12093 * t r2 = 0.601858
- Sweden
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 76.9362 + 0.13686 * t r2 = 0.921035
- United Kingdom
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 73.21921 + 0.19396 * t r2 = 0.961709
- USA
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 73.03983 + 0.19331 * t r2 = 0.984583
✹
❋✐❣✉r❡ ❆✺✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r c ♦❢ t❤❡ ▼❛❦❡❤❛♠ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00089 + −2e−05 * t r2 = 0.896826
- France
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00119 + −2e−05 * t r2 = 0.895841
- East Germany
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00128 + −2e−05 * t r2 = 0.801088
- West Germany
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00128 + −2e−05 * t r2 = 0.874556
- Hungary
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00163 + −3e−05 * t r2 = 0.955852
- Italy
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00157 + −3e−05 * t r2 = 0.823797
- Japan
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00115 + −2e−05 * t r2 = 0.739398
- Poland
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00175 + −3e−05 * t r2 = 0.885041
- Russia
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00149 + −1e−05 * t r2 = 0.616402
- Sweden
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00076 + −1e−05 * t r2 = 0.92755
- United Kingdom
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00098 + −2e−05 * t r2 = 0.856642
- USA
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00121 + −2e−05 * t r2 = 0.826258
✺
❋✐❣✉r❡ ❆✻✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r c ♦❢ t❤❡ ▼❛❦❡❤❛♠ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00124 + −2e−05 * t r2 = 0.868459
- France
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00169 + −3e−05 * t r2 = 0.94548
- East Germany
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00189 + −4e−05 * t r2 = 0.856536
- West Germany
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00187 + −4e−05 * t r2 = 0.906888
- Hungary
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00247 + −5e−05 * t r2 = 0.946038
- Italy
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00219 + −4e−05 * t r2 = 0.826553
- Japan
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00166 + −3e−05 * t r2 = 0.836608
- Poland
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00278 + −6e−05 * t r2 = 0.941738
- Russia
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00286 + −5e−05 * t r2 = 0.849257
- Sweden
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.0011 + −2e−05 * t r2 = 0.89661
- United Kingdom
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00128 + −2e−05 * t r2 = 0.83589
- USA
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00174 + −2e−05 * t r2 = 0.871132
✻
❋✐❣✉r❡ ❆✼✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r β ♦❢ t❤❡ ▼❛❦❡❤❛♠ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.10998 + −0.00019 * t r2 = 0.373413
- France
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.11164 + 0.00017 * t r2 = 0.811546
- East Germany
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.11665 + −4e−05 * t r2 = 0.037395
- West Germany
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.11404 + 6e−05 * t r2 = 0.188799
- Hungary
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.11885 + −0.00045 * t r2 = 0.882031
- Italy
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.11692 + 7e−05 * t r2 = 0.171529
- Japan
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.11423 + 0.00015 * t r2 = 0.600958
- Poland
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.11688 + −0.00022 * t r2 = 0.858631
- Russia
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.10639 + −0.00019 * t r2 = 0.603571
- Sweden
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.11377 + 9e−05 * t r2 = 0.359535
- United Kingdom
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.10491 + 7e−05 * t r2 = 0.151362
- USA
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.09886 + 5e−05 * t r2 = 0.149523
✼
❋✐❣✉r❡ ❆✽✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r β ♦❢ t❤❡ ▼❛❦❡❤❛♠ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.09903 + −5e−05 * t r2 = 0.0455
- France
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.09409 + −2e−05 * t r2 = 0.061623
- East Germany
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.1051 + −0.00026 * t r2 = 0.670178
- West Germany
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.09933 + 2e−05 * t r2 = 0.043333
- Hungary
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.1094 + −0.00079 * t r2 = 0.881155
- Italy
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.10017 + 7e−05 * t r2 = 0.111039
- Japan
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.10778 + −0.00014 * t r2 = 0.771795
- Poland
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.10688 + −0.00059 * t r2 = 0.942657
- Russia
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.08912 + −0.00053 * t r2 = 0.769739
- Sweden
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.10077 + 0.00017 * t r2 = 0.333842
- United Kingdom
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.09759 + 0.00012 * t r2 = 0.683517
- USA
Calendar year βt 1960 1980 2000 0.05 0.10 0.15 βt = 0.08688 + 0.00013 * t r2 = 0.568114
✽
❋✐❣✉r❡ ❆✾✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r M ♦❢ t❤❡ ▼❛❦❡❤❛♠ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 82.08159 + 0.08189 * t r2 = 0.899899
- France
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 81.86572 + 0.16947 * t r2 = 0.98857
- East Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 79.17722 + 0.15434 * t r2 = 0.835068
- West Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 80.34122 + 0.15407 * t r2 = 0.981722
- Hungary
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 80.03446 + 0.06289 * t r2 = 0.692389
- Italy
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 81.22247 + 0.16337 * t r2 = 0.977897
- Japan
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 79.73382 + 0.25001 * t r2 = 0.996258
- Poland
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 81.21003 + 0.07231 * t r2 = 0.759381
- Russia
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 83.14288 + −0.04837 * t r2 = 0.584253
- Sweden
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 82.32216 + 0.12657 * t r2 = 0.984331
- United Kingdom
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 81.16452 + 0.12048 * t r2 = 0.967259
- USA
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 82.67422 + 0.09927 * t r2 = 0.926296
✾
❋✐❣✉r❡ ❆✶✵✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r M ♦❢ t❤❡ ▼❛❦❡❤❛♠ ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 78.08186 + 0.06742 * t r2 = 0.63502
- France
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 75.77629 + 0.16386 * t r2 = 0.952521
- East Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 75.76599 + 0.10398 * t r2 = 0.580403
- West Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 75.55436 + 0.14724 * t r2 = 0.896129
- Hungary
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 77.28303 + −0.0666 * t r2 = 0.349709
- Italy
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 76.96812 + 0.14261 * t r2 = 0.857561
- Japan
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 76.32093 + 0.19261 * t r2 = 0.989976
- Poland
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 77.26946 + −0.01114 * t r2 = 0.027192
- Russia
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 77.52885 + −0.19778 * t r2 = 0.75616
- Sweden
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 78.43296 + 0.11402 * t r2 = 0.866932
- United Kingdom
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 75.13301 + 0.16328 * t r2 = 0.918643
- USA
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 76.01088 + 0.14812 * t r2 = 0.962156
✶✵
❋✐❣✉r❡ ❆✶✶✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r α ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.01481 + −0.00027 * t r2 = 0.827766
- France
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.01966 + −0.00041 * t r2 = 0.889581
- East Germany
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.023 + −5e−04 * t r2 = 0.8429
- West Germany
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.02405 + −0.00051 * t r2 = 0.900082
- Hungary
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.03956 + −0.00079 * t r2 = 0.951052
- Italy
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.03351 + −0.00075 * t r2 = 0.88483
- Japan
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.01714 + −0.00038 * t r2 = 0.762908
- Poland
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.03895 + −0.00078 * t r2 = 0.874919
- Russia
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.02548 + −0.00034 * t r2 = 0.870954
- Sweden
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.01216 + −0.00023 * t r2 = 0.918861
- United Kingdom
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.01881 + −0.00035 * t r2 = 0.943003
- USA
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.02076 + −0.00036 * t r2 = 0.902713
✶✶
❋✐❣✉r❡ ❆✶✷✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r α ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.02063 + −4e−04 * t r2 = 0.866703
- France
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.0259 + −0.00053 * t r2 = 0.892188
- East Germany
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.03048 + −0.00066 * t r2 = 0.861628
- West Germany
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.03113 + −0.00066 * t r2 = 0.901935
- Hungary
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.0498 + −0.001 * t r2 = 0.960404
- Italy
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.04151 + −0.00093 * t r2 = 0.89484
- Japan
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.02167 + −0.00048 * t r2 = 0.777935
- Poland
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.05098 + −0.00103 * t r2 = 0.896372
- Russia
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.0336 + −0.00044 * t r2 = 0.890512
- Sweden
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.01591 + −0.00031 * t r2 = 0.92229
- United Kingdom
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.0246 + −0.00046 * t r2 = 0.948025
- USA
Calendar year αt 1960 1980 2000 0.00 0.01 0.02 0.03 0.04 αt = 0.02708 + −0.00049 * t r2 = 0.894687
✶✷
❋✐❣✉r❡ ❆✶✸✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r β1 ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.89013 + −0.0071 * t r2 = 0.03801
- France
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 1.85621 + 0.08081 * t r2 = 0.82083
- East Germany
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.05578 + 0.03748 * t r2 = 0.316023
- West Germany
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.67809 + 0.01679 * t r2 = 0.520277
- Hungary
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 3.01919 + 0.00192 * t r2 = 0.005253
- Italy
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.10646 + 0.05764 * t r2 = 0.768362
- Japan
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 1.65777 + 0.02959 * t r2 = 0.446929
- Poland
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.69477 + 0.01209 * t r2 = 0.605331
- Russia
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 1.63302 + 0.02882 * t r2 = 0.593051
- Sweden
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 3.19862 + 0.0147 * t r2 = 0.065355
- United Kingdom
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.53588 + 0.011 * t r2 = 0.29938
- USA
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.64761 + 0.01477 * t r2 = 0.595391
✶✸
❋✐❣✉r❡ ❆✶✹✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r β1 ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.98791 + 0.00605 * t r2 = 0.028078
- France
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.64854 + 0.0369 * t r2 = 0.584791
- East Germany
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.53593 + 0.02684 * t r2 = 0.225381
- West Germany
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 3.15862 + 0.00301 * t r2 = 0.053864
- Hungary
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 3.28969 + −0.00257 * t r2 = 0.011657
- Italy
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.20995 + 0.08726 * t r2 = 0.873117
- Japan
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.24145 + 0.00445 * t r2 = 0.096979
- Poland
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 3.18772 + −0.00177 * t r2 = 0.020798
- Russia
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 1.8824 + 0.03053 * t r2 = 0.612237
- Sweden
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 3.5976 + 0.02848 * t r2 = 0.162399
- United Kingdom
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.48326 + 0.03108 * t r2 = 0.549872
- USA
Calendar year β1t 1960 1980 2000 2 3 4 5 6 β1t = 2.55707 + 0.05079 * t r2 = 0.800699
✶✹
❋✐❣✉r❡ ❆✶✺✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r c ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00035 + −1e−05 * t r2 = 0.912423
- France
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00046 + 0 * t r2 = 0.642852
- East Germany
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00048 + −1e−05 * t r2 = 0.772424
- West Germany
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00048 + −1e−05 * t r2 = 0.935611
- Hungary
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00044 + −1e−05 * t r2 = 0.945894
- Italy
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00044 + −1e−05 * t r2 = 0.725712
- Japan
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00052 + −1e−05 * t r2 = 0.56461
- Poland
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00044 + −1e−05 * t r2 = 0.912934
- Russia
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 5e−04 + 0 * t r2 = 0.002435
- Sweden
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00035 + 0 * t r2 = 0.88679
- United Kingdom
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00026 + 0 * t r2 = 0.611941
- USA
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00035 + 0 * t r2 = 0.736118
✶✺
❋✐❣✉r❡ ❆✶✻✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r c ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00045 + −1e−05 * t r2 = 0.839197
- France
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00047 + 0 * t r2 = 0.399031
- East Germany
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00068 + −1e−05 * t r2 = 0.897515
- West Germany
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00068 + −1e−05 * t r2 = 0.954182
- Hungary
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00062 + −2e−05 * t r2 = 0.810692
- Italy
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00054 + −1e−05 * t r2 = 0.462634
- Japan
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00078 + −1e−05 * t r2 = 0.831232
- Poland
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00067 + −2e−05 * t r2 = 0.898374
- Russia
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00052 + −1e−05 * t r2 = 0.685204
- Sweden
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00052 + −1e−05 * t r2 = 0.748346
- United Kingdom
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00027 + 0 * t r2 = 0.035619
- USA
Calendar year ct 1960 1980 2000 0.000 0.001 0.002 ct = 0.00037 + 0 * t r2 = 0.280128
✶✻
❋✐❣✉r❡ ❆✶✼✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r β2 ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.10472 + −0.00011 * t r2 = 0.193721
- France
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.10535 + 0.00028 * t r2 = 0.900815
- East Germany
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.11076 + 8e−05 * t r2 = 0.149705
- West Germany
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.10757 + 0.00019 * t r2 = 0.858201
- Hungary
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.10942 + −0.00029 * t r2 = 0.784829
- Italy
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.10741 + 0.00027 * t r2 = 0.896293
- Japan
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.10654 + 3e−04 * t r2 = 0.806327
- Poland
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.10514 + 0 * t r2 = 0.001122
- Russia
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09817 + −6e−05 * t r2 = 0.122872
- Sweden
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.10979 + 0.00015 * t r2 = 0.65897
- United Kingdom
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09969 + 0.00015 * t r2 = 0.540694
- USA
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09154 + 0.00016 * t r2 = 0.774832
✶✼
❋✐❣✉r❡ ❆✶✽✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r β2 ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09392 + 2e−05 * t r2 = 0.006774
- France
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.0868 + 9e−05 * t r2 = 0.626546
- East Germany
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09849 + −0.00014 * t r2 = 0.431435
- West Germany
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09264 + 0.00014 * t r2 = 0.861113
- Hungary
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09798 + −0.00053 * t r2 = 0.807106
- Italy
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09043 + 0.00028 * t r2 = 0.797062
- Japan
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09961 + 3e−05 * t r2 = 0.095232
- Poland
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09193 + −3e−04 * t r2 = 0.839832
- Russia
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.07487 + −0.00023 * t r2 = 0.525267
- Sweden
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09644 + 0.00024 * t r2 = 0.520638
- United Kingdom
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.09243 + 0.00019 * t r2 = 0.884473
- USA
Calendar year β2t 1960 1980 2000 0.05 0.10 0.15 β2t = 0.0794 + 0.00022 * t r2 = 0.835647
✶✽
❋✐❣✉r❡ ❆✶✾✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r M ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ❢❡♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 81.71862 + 0.08671 * t r2 = 0.896545
- France
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 81.38497 + 0.17916 * t r2 = 0.990649
- East Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 78.74069 + 0.16348 * t r2 = 0.857986
- West Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 79.88574 + 0.16335 * t r2 = 0.986945
- Hungary
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 79.33561 + 0.07325 * t r2 = 0.73997
- Italy
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 80.57278 + 0.17802 * t r2 = 0.986481
- Japan
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 79.27445 + 0.26077 * t r2 = 0.996285
- Poland
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 80.42819 + 0.08623 * t r2 = 0.81414
- Russia
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 82.47106 + −0.04007 * t r2 = 0.484208
- Sweden
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 82.06896 + 0.13077 * t r2 = 0.984016
- United Kingdom
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 80.68359 + 0.12857 * t r2 = 0.975938
- USA
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 82.00708 + 0.10974 * t r2 = 0.92512
✶✾
❋✐❣✉r❡ ❆✷✵✿ ❆♥♥✉❛❧ ❡st✐♠❛t❡s ❢♦r M ♦❢ t❤❡ ❙✐❧❡r ♠♦❞❡❧✱ ✇❤✐❝❤ ✐s ✜tt❡❞ t♦ ♠❛❧❡ ♠♦rt❛❧✐t② ❢♦r t❤❡ ❝❛❧❡♥❞❛r ②❡❛rs t✱ ✶✾✻✵ ✭❧✐❣❤t ❣r❛②✮ t♦ ✷✵✵✾ ✭❜❧❛❝❦✮✱ ❛❧♦♥❣ ✇✐t❤ ❛ ❧✐♥❡❛r r❡❣r❡ss✐♦♥ ✭s♦❧✐❞ ❧✐♥❡✮✱ ❢♦r ✶✷ ❝♦✉♥tr✐❡s ♦❢ t❤❡ ❍✉♠❛♥ ▼♦rt❛❧✐t② ❉❛t❛❜❛s❡ ✭✷✵✶✺✮
- Denmark
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 77.51541 + 0.07565 * t r2 = 0.690675
- France
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 74.79917 + 0.18193 * t r2 = 0.970508
- East Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 74.97315 + 0.11934 * t r2 = 0.653754
- West Germany
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 74.72269 + 0.16408 * t r2 = 0.929701
- Hungary
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 75.98925 + −0.0416 * t r2 = 0.156015
- Italy
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 75.84937 + 0.16773 * t r2 = 0.918548
- Japan
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 75.6716 + 0.20689 * t r2 = 0.98737
- Poland
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 75.77427 + 0.01183 * t r2 = 0.024912
- Russia
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 75.06638 + −0.15266 * t r2 = 0.685086
- Sweden
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 78.01548 + 0.12126 * t r2 = 0.881745
- United Kingdom
Calendar year Mt 1960 1980 2000 70 75 80 85 90 95 Mt = 74.45711 + 0.17492 * t r2 = 0.936506
- USA