Abstract
Abstract. The Non-Linear Mixed Spectral Finite-Difference (NLMSFD) model for surface boundary-layer flow over complex terrain has been extended to planetary boundary-layer flow over topography. Comparisons are made between this new version and the surface layer model. The model is also applied to simulate an Askervein experimental case. The results are discussed and compared with the observed field data.
Cite
CITATION STYLE
Weng, W., & Taylor, P. A. (2011). A Non-Linear Mixed Spectral Finite-Difference 3-D model for planetary boundary-layer flow over complex terrain. Advances in Science and Research, 6(1), 75–78. https://doi.org/10.5194/asr-6-75-2011
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