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Dry soils can intensify mesoscale convective systems
Soil moisture can feed back on rainfall through the impact of surface fluxes on the environment in which convection develops. The vast majority of previous research has focused on the initiation of convection, but in many regions of the world, the majority of rain comes from remotely triggered mesos...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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National Academy of Sciences
2020
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7474668/ https://www.ncbi.nlm.nih.gov/pubmed/32817526 http://dx.doi.org/10.1073/pnas.2007998117 |