Abstract
Theoretical results and data are presented in order to describethe spectral modifications induced by the effects of surfaceinhomogeneity on the features of turbulent boundary-layer flows.The hill case is used by way of example, and atmospheric andlaboratory data in neutral conditions are discussed. Shear andblocking effects with different characteristics are shown to bepresent both upwind and over the hill top.
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Tampieri, F., Mammarella, I. & Maurizi, A. Turbulence in Complex Terrain. Boundary-Layer Meteorology 109, 85–97 (2003). https://doi.org/10.1023/A:1025487702985
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DOI: https://doi.org/10.1023/A:1025487702985