forecasting wind energy variability using statistical downscaling techniques
DESCRIPTION
Peter Coppin European Wind Energy Conference March 2009. Forecasting Wind Energy Variability using Statistical Downscaling Techniques. Acknowledgements. Division of Marine and Atmospheric Research Robert Davy (principal researcher) Milton Woods Chris Russell Peter Coppin - PowerPoint PPT PresentationTRANSCRIPT
Forecasting Wind Energy Variability using Statistical Downscaling Techniques
Peter CoppinEuropean Wind Energy Conference March 2009
CSIRO. Forecasting Wind Energy Variability
Acknowledgements
Division of Marine and Atmospheric Research• Robert Davy (principal researcher)• Milton Woods• Chris Russell• Peter Coppin
Funded by the Australian Government – Department of Resources Energy and Tourism (DRET)
• Australia Wind Energy Forecasting System (supplied by ANEMOS)
In collaboration with• Australian Bureau of Meteorology• European Union Framework 7 “SAFEWIND” Project partners
CSIRO. Forecasting Wind Energy Variability
SE states 35,000MW max demand
Core wind generating area
CSIRO. Forecasting Wind Energy Variability
Typical winter / early spring conditions
CSIRO. Forecasting Wind Energy Variability
IR Satellite image – 1225 hr on Sept 11 2004 showing organised convection
CSIRO. Forecasting Wind Energy Variability
Example of problem – high variability in South Australia
High wind variability at moderate wind speeds
• large swings in aggregate wind power
• wind farm aggregation can amplify the absolute magnitude of power changes
• variation can exceed available spinning reserve response capability
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CSIRO. Forecasting Wind Energy Variability
Steps to forecasting wind variability
• Create a numerical index to describe severity
• Calculate index for observations
• Formally correlate observed variability with weather patterns derived from Numerical Weather Prediction (NWP) products via EOF analysis
• Produce prediction of variability based on combination of important patterns – using Random forest techniques – express in terms of wind speed and wind energy production ramp rate at suitable forecast time horizon
• Check predictability with observations (separate data segment)
CSIRO. Forecasting Wind Energy Variability
Modelling wind variability
Initial proof-of principle based on analysis fields (i.e. not forecast mode)
• NCEP Global Tropospheric Analyses ( ds083.2 )• six hourly meteorological fields at 1.0° resolution [1999 - ]
• Surface wind speed measurements: • 6 locations across South eastern Australia• Used for calculating variability index and validation
Forecast mode trial
• Bureau of Meteorology W-LAPS model• Six hourly fields at 1° and 0.1° grids (data set length?)• 12 hours ahead
CSIRO. Forecasting Wind Energy Variability
Index of wind variability
• from Woods, Davy & Coppin, 2007• Variability index is six hour running standard deviation of 2 hour
high-pass filtered (10min) raw data-5
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Original dataFluctuationsVariability index
CSIRO. Forecasting Wind Energy Variability
Available (and relevant) variables for EOF analysis
• NCEP Global Tropospheric Analyses ( ds083.2 )• six hourly meteorological fields at 1.0° resolution [1999 - ]
Geopotential height Air temperature Relative humidityU wind speedV wind speedVertical velocityAbsolute vorticityHeight of planetary boundary layerPrecipitable waterCloud waterLifting indexConvective inhibitionConvective available potential energyetc
CSIRO. Developing a prediction of wind variability
EOF example : Temperature-2
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CSIRO. Forecasting Wind Energy Variability
Quantitative modelling
Meteorological inputs(transformed using EOF)
Empirical model(random forest)
Sum of variability indexat 6 sites
Model period: 2003-4
CSIRO. Forecasting Wind Energy Variability
Winter – important patterns explaining variability
Height of planetary boundary layer – EOF1 Absolute vorticity – EOF3
Velocity component V – EOF2
CSIRO. Forecasting Wind Energy Variability
NCEP Results – winter / early spring
• Prediction of variability index (using analysis NWP products)
Important predictors:EOF number
Height of planetary boundary layer 1Absolute vorticity 3V wind speed 2U wind speed 1
R2=0.74
Aggregate 6 locations in SE Australia
CSIRO. Forecasting Wind Energy Variability
NCEP Results – winter / early spring
• Prediction of variability index (using analysis NWP products)
Important predictors:EOF number
Height of planetary boundary layer 1Absolute vorticity 3V wind speed 2U wind speed 1
R2=0.74
Single siteAggregate 6 locations in SE Australia
CSIRO. Forecasting Wind Energy Variability
Summer – important patterns explaining variability
Geopotential height – EOF2
Convective available potential energy – EOF1Cloud water – EOF1
CSIRO. Forecasting Wind Energy Variability
NCEP Results - summer
• Prediction of variability index (using analysis NWP products)
Important predictors:EOF number
Cloud water 1Geopotential height 2CAPE 1V wind speed 2
R2=0.66
Aggregate 6 locations in SE Australia
CSIRO. Forecasting Wind Energy Variability
NCEP Results - summer
• Prediction of variability index (using analysis NWP products)
Important predictors:EOF number
Cloud water 1Geopotential height 2CAPE 1V wind speed 2
R2=0.66
Single siteAggregate 6 locations in SE Australia
CSIRO. Developing a prediction of wind variability
Modelling of 6-hour mean ramp rate • aggregate power from 6 locations vs fitted variability index
Mean wind power ramp rate modelling
CSIRO. Forecasting Wind Energy Variability
Short-term wind power ramp rate modelling
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Modelling of 10 min ramp rate
•aggregate power from 6 locations (normalised)
•relationship of 6 hourly maximum ramp rate (left) and instantaneous ramp rate (right) to variability index
CSIRO. Forecasting Wind Energy Variability
W-LAPS forecast mode trial
• EOF analysis uses both 1° (100km) and 0.1° (10km) fields
• Correlations performed on 12-hour ahead forecast products
• Single site results available
• Example EOF model fit:
Variable Grid domain EOF number
Vertical velocity (omega) Inner 1
Mean sea level pressure Inner 3
24 hour precipitation Inner 1
Latent heat flux Outer 2
Atmospheric boundary layer height
Outer 2
CSIRO. Forecasting Wind Energy Variability
W-LAPS Results – 12 hours ahead
• Forecast of variability index (using analysis NWP products)• Single site
Winter Summer
CSIRO. Forecasting Wind Energy Variability
W-LAPS Results – 12 hours ahead
• Forecast of variability index (using analysis NWP products)• Aggregate of several sites in one state
Winter Summer
CSIRO. Forecasting Wind Energy Variability
Further work
• Implement working system• ready for coding into ANEMOS system as a module
• Further validate forecast-mode models for aggregate variability• requires additional surface data
• Quantify value to system operators of variability information• cost benefit analysis
Contact UsPhone: 1300 363 400 or +61 3 9545 2176
Email: [email protected] Web: www.csiro.au
Thank you
Centre for Australian Weather and Climate ResearchA partnership between CSIRO and the Bureau of MeteorologyRobert Davy
Phone: 02 6246 5604Email: [email protected]: www.csiro.au/weru