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- W1676230691 abstract "Basically, energetics in an atmospheric boundary layer (ABL) without energy extraction by turbines is simple: The potential energy (PE) of the pressure-field is transformed to kinetic energy (KE) of the wind by down-gradient volume-flow. KE is further transformed to turbulent KE (TKE), which is dissipated to heat by viscous processes at the smallest turbulence scales. In stable stratification, a small fraction of the TKE is transformed to PE by mixing the stratified fluid. Energy-extraction by turbines is primarily on expense of the KE, but especially in large-scale utilisation there are necessarily also effects on TKE and dissipation. If the large-scale input of PE to the ABL is a constant, which is a reasonable first assumption, dissipation must become smaller by the amount of extracted energy, and thus also TKE as source for dissipation processes must become smaller. This is in contradiction to the usual conception that turbines increase the turbulence. Open questions: Is the variability added by the turbines really turbulence? If it is – where does all the energy come from?" @default.
- W1676230691 created "2016-06-24" @default.
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- W1676230691 date "2010-05-01" @default.
- W1676230691 modified "2023-09-28" @default.
- W1676230691 title "Large-Scale Wind-Energy Utilisation and Some Open Questions in Atmospheric-Boundary-Layer Energetics" @default.
- W1676230691 hasPublicationYear "2010" @default.
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