Wind-tunnel simulation of stably stratified atmospheric boundary layers
Wind-tunnel simulation of stably stratified atmospheric boundary layers
复制标题
稳定分层大气边界层的风洞模拟
DOI：
10.1088/1742-6596/753/3/032012
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发表时间：
2016
期刊：
影响因子：
--
通讯作者：
Hancock P
中科院分区：
文献类型：
--
作者：
Hancock P
Results are presented of simulations of a stable boundary layer of moderate surface condition and zero overlying inversion strength. The layer depth is matched to model scale by artificially thickening the boundary layer by means of flow generators ('spires') at the working-section inlet. A non-uniform inlet temperature profile is essential in order to preclude the upper part of the layer retaining neutral conditions. The layer behaviour is sensitive to the prescribed form and care is needed in its specification. The results also show that the surface cooling should be started some distance downstream of the working-section inlet. The developed flow is closely horizontally homogeneous.
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