4.0 Article

Analysis of diabatic flow modification in the internal boundary layer

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METEOROLOGISCHE ZEITSCHRIFT
卷 20, 期 6, 页码 649-659

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E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG
DOI: 10.1127/0941-2948/2011/0290

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资金

  1. Danish Research Agency
  2. Strategic Research Council
  3. Program for Energy and Environment [Sagsnr. 2104-08-0025]
  4. EU [TREN-FP7EN-219048, PIEF-GA-2009-237471-VSABLA]

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Measurements at two meteorological masts in Denmark, Horns Rev in the sea and Hovsore near the coastline on land, are used to analyze the behaviour of the flow after a smooth-to-rough change in surface conditions. The study shows that the wind profile within the internal boundary layer is controlled by a combination of both downstream and upstream stability and surface roughness conditions. A model based on a diffusion analogy is able to predict the internal boundary layer height well. Modeling the neutral and long-term wind profile with a 3 layer linear interpolation scheme gives good results at Hovsore. Based on a comparison with a numerical model and the measurements, the constants in the interpolation scheme are slightly adjusted, which yields an improvement for the description of the wind profile in the internal boundary layer.

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