2022
DOI: 10.1127/metz/2022/1109
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Coastal impacts on offshore wind farms – a review focussing on the German Bight area

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Cited by 10 publications
(10 citation statements)
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“…There are several pronounced features: Wind from the South-West sector was frequently associated with a wind speed between 5 m s −1 and 15 m s −1 . This corresponds to the most frequent wind direction for the North Sea (Platis et al, 2018), and is typically associated with stable conditions in spring and summer (Schulz-Stellenfleth et al, 2022). Further, conditions with wind directions from East were measured, which is also typically associated with stable conditions.…”
Section: Wind Directionmentioning
confidence: 85%
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“…There are several pronounced features: Wind from the South-West sector was frequently associated with a wind speed between 5 m s −1 and 15 m s −1 . This corresponds to the most frequent wind direction for the North Sea (Platis et al, 2018), and is typically associated with stable conditions in spring and summer (Schulz-Stellenfleth et al, 2022). Further, conditions with wind directions from East were measured, which is also typically associated with stable conditions.…”
Section: Wind Directionmentioning
confidence: 85%
“…The phenomenon of the coastal transition was another target of the measurement flights. The coastal effect means that the abrupt changes of the surface properties at the coast, with lower surface roughness and different heat capacity, lead to modifications of the wind field and the thermal stratification (Schulz-Stellenfleth et al, 2022), which is particularly challenging to include in simulations (Siedersleben et al, 2018). The increase or decrease of wind speed due to synoptic scale changes and the coastal effect can be in the order of several m s −1 (e.g., Platis et al, 2018;Djath et al, 2022).…”
Section: Flight Planning and Flight Patternsmentioning
confidence: 99%
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“…In coastal regions, LLJ, characterized by a maximum in the wind speed profile in the lower troposphere [7,8], can have different driving mechanisms [9]. According to Schulz-Stellenfleth et al [10], LLJ can be attributed to frictional decoupling from the underlying surface or baroclinicity due to the temperature contrast between the land and sea. Over the southern North Sea, relatively warm continental air advected over the cooler sea surface supports the development of surface temperature inversion, leading to the decoupling of the surface friction and acceleration of an air mass [11,12].…”
Section: Introductionmentioning
confidence: 99%