How an extrem e w ind atlas is m ade AC Kruger South African - - PowerPoint PPT Presentation

how an extrem e w ind atlas is m ade
SMART_READER_LITE
LIVE PREVIEW

How an extrem e w ind atlas is m ade AC Kruger South African - - PowerPoint PPT Presentation

How an extrem e w ind atlas is m ade AC Kruger South African Weather Service X Larsn DTU Wind Energy Wind Atlas for South Africa (WASA) 1 Why do we need extreme wind statistics? Statistical background for estimation of extreme


slide-1
SLIDE 1

Wind Atlas for South Africa (WASA)

How an extrem e w ind atlas is m ade

AC Kruger – South African Weather Service X Larsén – DTU Wind Energy

1

slide-2
SLIDE 2

Wind Atlas for South Africa (WASA) 2

  • Why do we need extreme wind statistics?
  • Statistical background for estimation of extreme wind

stats

  • Development of extreme wind statistics/values

– measured data – modelling

  • Applications
  • wind energy
  • built environment
  • disaster management
slide-3
SLIDE 3

Wind Atlas for South Africa (WASA)

W hy do w e need extrem e w ind statistics?

  • Information on extreme winds essential in the design of wind farms – situated

in areas with relatively strong winds;

  • Application of REWC to obtain extreme wind statistics for wind farm position

(e.g. with WAsP Eng.) for IEC 61400-1;

  • Updated extreme wind statistics critical for optimal design of built

environment

  • Disaster management – strong wind hazard profiles for risk estimation

3

slide-4
SLIDE 4

Wind Atlas for South Africa (WASA)

Statistical Approaches

Annual maxima – most widely applied: GEV (3 types: k < 0, k = 0 (Gumbel) and k >0) Shortcomings of GEV approach:

  • Only one maximum value selected per epoch (per annum)
  • Data sets must be long (>= 20 years)
  • Cannot be used for data sets < 10 years

Alternative approaches to increase number of cases, e.g.:

  • r-largest values per epoch
  • Method of Independent Storms (MIS)
  • Peak Over Threshold (POT)
slide-5
SLIDE 5

Wind Atlas for South Africa (WASA)

Mixed strong wind climates:

  • Mixed distribution method – storms from different origins to

be considered separately

  • Return period values from combination of set of Gumbel

distributions

Hourly Mean Gust

slide-6
SLIDE 6

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA)

6

Estim ation of Extrem e W ind Statistics for South Africa

slide-7
SLIDE 7

Wind Atlas for South Africa (WASA)

Analysis of m easured data

7

slide-8
SLIDE 8

Wind Atlas for South Africa (WASA)

Modeling

  • High spatial resolution possible;
  • New methods continuously researched:

Low tim e-resolution data ( e.g. 6 -hourly w ind speed) High tim e-resolution statistics ( e.g. 1 :5 0 yr 1 0 m in w ind speed)

8

  • Temporal variability can be missed out by smoothing

effect of numerical modelling;

slide-9
SLIDE 9

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA) WASA workshop April 2014

9

Selective Dynam ical Dow nscaling Method ( SDDM)

STEP 1 : I dentification of annual m ax. storm s STEP 2 : Mesoscale m odelling of storm s:

1. Run WRF for the 72+175 cases

  • Input: CFSR data, 6 hrly, 1998 -

2010

  • 20 s time step
  • 41 vertical layers
  • Run time <=72 hrs per storm
  • 4 km resolution
  • Output: 10 min

2. The 50-year wind using the Annual Maxima Method (Gumbel distribution).

slide-10
SLIDE 10

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA)

1

  • Correction to the standard condition:

Height: 10 m, Roughness length: 5 cm

  • Microscale generalisation scheme with Linear Computational Model (LINCOM) to
  • btain mesoscale speedup factors from upwind orography and roughness length

Larsén et al. (2013): The selective dynamical downscaling method for extreme wind atlases, Wind Energy, 2013; 16:1167–1182.

STEP 3 : Post-processing procedure:

slide-11
SLIDE 11

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA)

  • E.g. Brausseur’s concept of the gust and estimation:
  • Classical gust calculation: Wind converted to 10 min, application of

turbulence model to obtain gust

11

Gust m odelling

(Larsén and Kruger: Extreme gust wind estimation using mesoscale modeling, in Proceedings of European Wind Energy Associations, 10 – 13 March, 2014, Barcelona Spain.)

Basis: Modelling of air parcels deflected to the surface through turbulent eddies:

slide-12
SLIDE 12

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA)

12 1: 50 year 1 0 -m in wind at 10 m over roughness length = 5 cm Horizontal resolution: 4 km

22 23 24 25 26 27 28 29

  • 35
  • 34.5
  • 34
  • 33.5
  • 33
  • 32.5
  • 32
  • 31.5

Longitude o 1 2 2 3 3

SDDM Outputs:

slide-13
SLIDE 13

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA)

13 Gust estim ations through m odelling:

slide-14
SLIDE 14

Wind Atlas for South Africa (WASA)

14 Com parison betw een m easurem ents and m odelling ( e.g. 1 0 m in) :

slide-15
SLIDE 15

Wind Atlas for South Africa (WASA) Sep 2013

5 5 4 5 3 5 2 5 15 20 25 30 35

15

slide-16
SLIDE 16

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA)

16 Final 1 0 m in m ap ( Measurem ents + SDDM) : Upw ard adjustm ents of m odelled values w here necessary

slide-17
SLIDE 17

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA)

17

slide-18
SLIDE 18

Wind Atlas for South Africa (WASA)

Checklist

  • Extreme winds
  • Turbulence Intensity
  • Vertical wind shear
  • Flow inclination
  • Wake turbulence

Vref : Hub-height, 10-min, 1: 50 yr extreme wind Iref : Reference turbulence intensity at 15 m/ s in a 10-min period

W ind farm planning: Application of appropriate software (e.g. WAsP Engineering) with inputs e.g.:

  • Extreme wind statistics (REWC),
  • Information of the wind farm (e.g. arrangement of wind turbines),
  • Environment around the proposed wind farm (e.g. surface roughness,

topography and obstacles).

  • IEC 61400-1 site assessment rules:

Applications

slide-19
SLIDE 19

Wind Atlas for South Africa (WASA)

Built environm ent:

Update of SABS SANS 1 0 1 6 0 -3 W ind Actions:

  • Fundamental value of basic wind speed vb,0:

Intervals range from 32 m/ s (green), to 44 m/ s (red)

  • Based on measured values, but with WASA 1 modelling results considered
  • Details in forthcoming suite of 4 papers (SAICE journal)

Applications

slide-20
SLIDE 20

Wind Atlas for South Africa (WASA)

Disaster m anagem ent:

  • Quantification of wind hazard used in the relative assessment of risk (1:

lowest – 5: highest), quantitatively defined as risk= ( hazard× vulnerability) / capacity

  • Risk includes 4 factors defined by NDMC:

1. Likelihood 2. Frequency 3. Magnitude 4. Predictability

  • Wind hazard: Wind gust > 20 m/ s – damage to infrastructure possible

(Kruger et al. 2016 - SAJS)

  • As with loading code – wind hazard identified per local municipality to

identify vulnerable local government areas:

Applications

slide-21
SLIDE 21

Wind Atlas for South Africa (WASA)

Likelihood: Frequency: Magnitude: Predictability:

slide-22
SLIDE 22

Wind Atlas for South Africa (WASA)

Relative wind hazard (incl. of 4 factors) - seasonal:

slide-23
SLIDE 23

Wind Atlas for South Africa (WASA)

Relative wind hazard (annual):

slide-24
SLIDE 24

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA)

Additional inform ation:

  • WASA 1 guidelines for using extreme wind data (application of WAsP

Eng.) and how to obtain the data: www.wasainfo.org

  • Climatic background to strong winds & estimation of extreme wind

statistics from measured data: Kruger, A.C. Wind climatology of South Africa relevant to the design of the built environment. PhD dissertation, 2011, Stellenbosch University. http://hdl.handle.net/10019.1/6847.

  • Modelling approaches and results:

1. Larsén, X.G., Kruger A.C., Badger, J. and Jørgensen, H.E. 2013a. Extreme wind atlases of South Africa from global reanalysis data. Proceedings of the Europe Africa Conference on Wind Engineering, Cambridge, July 2013. 2. Larsén, X.G., Kruger, A.C., Badger, J. and Jørgensen, H.E. 2013b. Dynamical and statistical downscaling approaches for extreme wind atlas of South Africa. Proceedings of the European Meteorological Society Conference, Reading, UK, September 2013. 3. Larsén, X.G. and Kruger, A.C. Application of the spectral correction method to reanalysis data in South Africa. Journal of Wind Engineering and Industrial Aerodynamics, 2013, 133: 110-122. 4. Larsén, X.G. and Kruger, A.C. Extreme gust wind estimation using mesoscale modelling. Proceedings of the European Wind Energy Associations, 10 – 13 March, 2014, Barcelona Spain.

slide-25
SLIDE 25

Wind Atlas for South Africa (WASA) Wind Atlas for South Africa (WASA)

Additional inform ation:

  • Wind loading code:

1. Kruger et al. 2013a. Kruger A. C., Retief, J.V., Goliger, A. M. 2013. Strong winds in South Africa: Part I – Application of estimation methods. Journal of the South African Institution

  • f Civil Engineering.

2. Kruger A. C., Retief, J.V., Goliger, A. M. Strong Winds in South Africa: Part II - Mapping

  • f Updated Statistics. 2013. Journal of the South African Institution of Civil Engineering.

3. Retief, J.V. and P. E. Dunaiski (ed.). Goliger, A. M., J. V. Retief, P.E. Dunaiski and A. C.

  • Kruger. 2009. Revised wind-loading procedures for SANS 10160. In “Background to

SANS 10160. Basis of Structural Design and Actions for Buildings and Industrial Structures.”, SunMedia, Stellenbosch. 4. Forthcoming set of papers in Journal of the South African Institution of Civil Engineering detailing development, application and consideration of uncertainties.

  • Disaster management:

Kruger, A.C. et al. 2016. Indicative hazard profile for strong winds in South Africa. South African Journal of Science.