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Research and esearch and d development evelopment R in connection with climate change in connection with climate change at Hungarian Meteorological Service at Hungarian Meteorological Service Zolt n Dunkel dr. n Dunkel dr. Zolt


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SLIDE 1

R Research and esearch and d development evelopment in connection with climate change in connection with climate change at Hungarian Meteorological Service at Hungarian Meteorological Service

Zolt Zoltá án Dunkel dr. n Dunkel dr. President of Hungarian Meteorological Service President of Hungarian Meteorological Service dunkel.z@ met.hu dunkel.z@ met.hu

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  • On the base of homogenized daily

data series for temperature and precipitation: 1901- 2010

  • Analysis of mean parameters and

climate extremes

Analysis of observed tendencies Analysis of observed tendencies

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SLIDE 3

Annual Annual temperature averages and temperature averages and the fitted trends to the period 1901 the fitted trends to the period 1901-

  • 2010 and 1981

2010 and 1981-

  • 2010

2010

Observed temperature changes °C year spring summer autumn winter 1901‐2010 0.98 1.1 1.2 0.65 0.64 1981‐2010 1.17 1.3 1.7 0.66 0.8

Sinificant changes are bolded

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SLIDE 4

Observed precipitation changes % year spring summer autumn winter 1901‐2010 ‐5% ‐17% 11% ‐14% 1% 1981‐2010 25% 13% 36% 30% 12%

Sinificant changes are bolded

Annual precipitation sum Annual precipitation sum and the fitted trends to the period and the fitted trends to the period 1901 1901-

  • 2010

2010

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SLIDE 5

Change of the temperature, 1980-2009 1.06°C 1.52°C 2.07°C min mean max Change of the precipitation, 1960-2009

  • 22.00%
  • 1.70%

21.00% min mean max

Change of the annual temperature Change of the annual temperature and precipitation and precipitation

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SLIDE 6

Extreme climate indices: Extreme climate indices:

  • bserved changes 1901
  • bserved changes 1901-
  • 2009

2009

20 40 60 80 100 120 140 1901 1911 1921 1931 1941 1951 1961 1971 1981 1991 2001

Trend= 0.8days/decade

40 60 80 100 120 140 160 1901 1911 1921 1931 1941 1951 1961 1971 1981 1991 2001

Trend= -1 days/decade

1 2 3 4 5 6 1901 1911 1921 1931 1941 1951 1961 1971 1981 1991 2001

Trend= 0.1 days/decade

5 10 15 20 25 30 35 40 45 1901 1911 1921 1931 1941 1951 1961 1971 1981 1991 2001

Trend= -0.4% /decade

10 15 20 25 30 35 40 45 50 1901 1911 1921 1931 1941 1951 1961 1971 1981 1991 2001

Trend=0.4days/decade

3 4 5 6 7 8 9 10 11 1901 1911 1921 1931 1941 1951 1961 1971 1981 1991 2001

Summer Trend=0.12 mm/decade

Frost days: Tmin < 0 °C Summer days: Tmax > 25 °C Warm nights: Tmin > 20 °C

% of wet days: daily precipitation > 1 mm Simple daily intensity: precipitation sum/number

  • f wet days

Maximum number of consecutive days when the daily precipitation < 1 mm

Temperature Precipitation

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SLIDE 7
  • Two models:

Two models:

ALADIN-Climate REMO Period 1961–2100 1951–2100 Resolution 10 km and 31 levels 25 km and 20 levels Scenario A1B A1B

Climate modelling Climate modelling

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SLIDE 8

Changes in temperature Changes in temperature Annual mean, reference period 1961 Annual mean, reference period 1961-

  • 1990

1990

Significant changes: Warming in each seasons, most effective in summer and autumn Increasing number of heat days, hot days and heat waves

2021- 2050 2071- 2100 ALADIN- Climate REMO

1.4- 1.9°C 3.5- 3.9°C

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SLIDE 9

Changes in precipitation Changes in precipitation Annual sum, reference period 1961 Annual sum, reference period 1961-

  • 1990

1990

Not significant changes in general Greater uncertainty than at the temperature Change within the year Summer: increacing, other seasons: depend on the models Increasing intensity (significant for 2071–2100) Increasing number of the consecutive dry days for 2071- 2100

2021- 2050 2071- 2100 ALADIN- Climate REMO

(- 1)- 0% (- 5)- (+ 3)%

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SLIDE 10

Thank you for your attention! Thank you for your attention!