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Coupling with ocean mixed layer leads to intraseasonal variability in tropical deep convection: Evidence from cloud‐resolving simulations

Abstract The effect of coupling a slab ocean mixed layer to atmospheric convection is examined in cloud‐resolving model (CRM) simulations in vertically sheared and unsheared environments without Coriolis force, with the large‐scale circulation parameterized using the Weak Temperature Gradient (WTG)...

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-д хадгалсан:
Номзүйн дэлгэрэнгүй
Үндсэн зохиолчид: Usama Anber, Shuguang Wang, Adam Sobel
Формат: Artigo
Хэл сонгох:Inglês
Хэвлэсэн: American Geophysical Union (AGU) 2017-03-01
Цуврал:Journal of Advances in Modeling Earth Systems
Нөхцлүүд:
Онлайн хандалт:https://doi.org/10.1002/2016MS000803
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