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An Observational Overview of Dusty Deep Convection in Martian Dust Storms
Deep convection, as used in meteorology, refers to the rapid ascent of air parcels in the Earth’s troposphere driven by the buoyancy generated by phase change in water. Deep convection undergirds some of the Earth’s most important and violent weather phenomena and is responsible for many aspects of...
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| Publicado no: | J Atmos Sci |
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| Main Authors: | , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
2019
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7446947/ https://ncbi.nlm.nih.gov/pubmed/32848258 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1175/jas-d-19-0042.1 |
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