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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...

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Pubblicato in:Proc Natl Acad Sci U S A
Autori principali: Klein, Cornelia, Taylor, Christopher M.
Natura: Artigo
Lingua:Inglês
Pubblicazione: National Academy of Sciences 2020
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Accesso online:https://ncbi.nlm.nih.gov/pmc/articles/PMC7474668/
https://ncbi.nlm.nih.gov/pubmed/32817526
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2007998117
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