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Turbulent kinetic energy over large offshore wind farms observed and simulated by the mesoscale model WRF (3.8.1)
Ist Teil von
Geoscientific Model Development, 2020-01, Vol.13 (1), p.249-268
Ort / Verlag
Katlenburg-Lindau: Copernicus GmbH
Erscheinungsjahr
2020
Link zum Volltext
Quelle
EZB Electronic Journals Library
Beschreibungen/Notizen
Wind farms affect local weather and microclimates;
hence, parameterizations of their effects have been developed for numerical weather prediction models.
While most wind farm parameterizations (WFPs) include drag effects of wind farms, models differ on whether or not an additional
turbulent kinetic energy (TKE) source should be included in these
parameterizations to simulate the impact of wind farms on the boundary layer.
Therefore, we use aircraft measurements above large offshore wind farms in stable conditions to evaluate
WFP choices. Of the three case studies we examine, we find the simulated ambient background
flow to agree with observations of temperature stratification and winds. This agreement allows us to
explore the sensitivity of simulated wind farm effects with respect to modeling choices
such as whether or not to include a TKE source, horizontal resolution, vertical resolution
and advection of TKE. For a stably stratified marine atmospheric boundary layer (MABL), a TKE source and a horizontal resolution
on the order of 5 km or finer are necessary to represent the impact of offshore wind farms on the MABL.
Additionally, TKE advection results in excessively reduced TKE over the wind farms, which in turn causes
an underestimation of the wind speed deficit above the wind farm. Furthermore, using fine vertical
resolution increases the agreement of the simulated wind speed with satellite observations of surface wind speed.