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)...
Wedi'i Gadw mewn:
| Prif Awduron: | , , |
|---|---|
| Fformat: | Artigo |
| Iaith: | Inglês |
| Cyhoeddwyd: |
American Geophysical Union (AGU)
2017-03-01
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| Cyfres: | Journal of Advances in Modeling Earth Systems |
| Pynciau: | |
| Mynediad Ar-lein: | https://doi.org/10.1002/2016MS000803 |
| Tagiau: |
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