Gradient -diffusion closure and the ejection -sweep cycle in convective boundary layers
The inadequacy of conventional gradient -diffusion closure in modeling turbulent heat flux within the convective atmosphe ric boundary -layer is often alleviated by accounting for nonlocal transport. Such nonlocal effects are a manifestation of the inherent asy mmetry in vertical tr...
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| Vydáno v: | Ciência e Natura |
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| Hlavní autoři: | , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universidade Federal de Santa Maria
2016
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=467547689089 |
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