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2015
DOI: 10.1007/s10546-015-0008-x
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On the Offshore Advection of Boundary-Layer Structures and the Influence on Offshore Wind Conditions

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Cited by 60 publications
(64 citation statements)
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References 25 publications
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“…Accordingly, the turbines near this corner of the wind farm are the ones closest to the shore. Since the wind speed tends to increase with increasing distance from the coast [10,11], the increase in the wind speed from the northwest corner moving east along the northern face of Rødsand II is consistent with what one would expect from the shape of the coastline and the layout of the wind farm. In contrast, the northernmost row of Nysted is almost parallel with the coastline, and there is little variation in the inflow wind speeds from the north.…”
Section: Coastal Effectssupporting
confidence: 78%
“…Accordingly, the turbines near this corner of the wind farm are the ones closest to the shore. Since the wind speed tends to increase with increasing distance from the coast [10,11], the increase in the wind speed from the northwest corner moving east along the northern face of Rødsand II is consistent with what one would expect from the shape of the coastline and the layout of the wind farm. In contrast, the northernmost row of Nysted is almost parallel with the coastline, and there is little variation in the inflow wind speeds from the north.…”
Section: Coastal Effectssupporting
confidence: 78%
“…the horizontal wind speed gradient due to a varying distance to shore (fetch), and wind farm wakes from other wind farms both influence the wind resource. Dörenkämper et al (2015) found that large "horizontal streaks of reduced wind speeds that under stable stratification are advected several tens of kilometres over the sea" can severely affect offshore wind farms. Correct prediction of the wind resource influenced by either land or adjacent wind farms, or a combination of the two, is a challenging problem.…”
Section: Introductionmentioning
confidence: 99%
“…In this study we will investigate possible creation mechanisms of boundary layer rolls that exist in the coastal zone. Other types of streaky structures elongated in the along-wind direction have also been observed and can be formed by lee effects from terrain [1] or from orography inhomogeneities [2]. In these types of features, however, each streak is created from a certain source, behaving like a wake.…”
Section: Introductionmentioning
confidence: 99%