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Abstract
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| We have reproduced the Bolund experiment in a wind tunnel for a 270º wind direction, and we predict that the region of high TKE generated at the edge of the escarpment does not evolve downstream on the plateau uniformly. Instead, two longitudinal regions of high TKE and low speed are developed surrounding a central region of high speed and low TKE. At least for one of these two regions, the presence of a longitudinal vortex-like structure has been observed in the mean velocity field. High cross-flow gradients in the mean speed and TKE fields are observed across these three regions. | |
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International
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Si |
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Congress
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EWEA 2014 Annual Event |
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960 |
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Place
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Copenhagen |
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Reviewers
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Si |
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ISBN/ISSN
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Start Date
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10/03/2014 |
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End Date
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13/03/2014 |
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From page
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To page
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EWEA 2014 Annual Event |