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TECHNICAL



        Regional climatology is generally derived from historic large-scale
        wind data sources. The generalised wind climatology process is
        derived from mesa or large-scale weather data, obtained from
        weather monitoring sources and validated by ground-based
        stations.
           The extrapolation process requires a detailed knowledge of the
        terrain surrounding the site and the effect of topological features
        on wind speed. Begun in 2010, the project consisted of three
        phases, WASA1, 2 and 3. WASA 3 was concluded in October 2021.

        There are two processes involved which run concurrently:
        modelling and verification

        MESOscale modelling
        Mesoscale modelling involves construction of a model based on
        macroscale (global) wind patterns, using knowledge of wide area
        terrain features to scale down to a MESOscale (regional) wind
        pattern (using 100 km blocks), in this case the Weather Research
        and Forecasting (WRF) model. The mesoscale model uses a
        variety of global, geophysical and meteorological databases such
        as the Reanalysis database. This database is a gridded historical
        weather data set produced by many weather bureaus or research
        centres across the globe. WRF is a numerical weather prediction
        (NWP) system designed to serve both atmospheric research and
        operational forecasting needs which allows for the production of
        simulations reflecting either real data (observations, analyses) or
        idealized atmospheric conditions.
           Figure 3 shows a Mesoscale WRF wind map showing long term
        averaged wind speeds at a height of 100 m AGL.
                                                               Figure 4: WASA high resolution wind resource map: Mean wind speed
                                                               [ms ] @ 100 m a.g.l., December 2020 (3,3 km WRF + 250 m WAsP
                                                                  -1
                                                               modelling) 3


                                                               Verification
                                                               In parallel with this program there is a physical wind speed
                                                               measurement and recording program, using specifically designed
                                                               masts installed at specially chosen sites around the country. Data
                                                               from the masts is used to validate the calculated values (Figure 5).






        Figure 3: Mesoscale wind map 3


        Microscale modelling
        MESOscale data is used as input to the WAsP computer program
        which produces microscale wind data using detailed data on
        roughness, orography and obstacles. The WAsP program typically
                                         2
        produces wind pattern data in areas of 250 m . WAsP is a software
        package used to evaluate the wind potential at specific sites,
        developed by the Danish Technical University, and capable of
        estimating site wind potential based on higher level input from
        either observations or local climate models (WRF). WAsP was used
        in developing the WASA.                                Figure 5: Location of the wind monitoring masts 3



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