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A Note on Scalar-Gradient Sharpening in the Stable Atmospheric Boundary Layer
The scalar front generated by the horizontal self advection of a dipolar vortex through a modest scalar gradient is investigated. This physical scenario is an idealization of the emergence of strong temperature ramps in the stable atmospheric boundary layer. The proposed mechanism is discussed and a...
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Springer Netherlands
2020
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7242271/ https://www.ncbi.nlm.nih.gov/pubmed/32508348 http://dx.doi.org/10.1007/s10546-020-00516-x |