Tropical Deep Convection, Cloud Feedbacks and Climate Sensitivity
This paper is concerned with how the diabatically-forced overturning circulations of the atmosphere, established by the deep convection within the tropical trough zone (TTZ), first introduced by Riehl and (Malkus) Simpson, in Contr Atmos Phys 52:287–305 (1979), fundamentally shape the distributions...
المؤلفون الرئيسيون: | Stephens, GL, Shiro, KA, Hakuba, MZ, Takahashi, H, Pilewskie, JA, Andrews, T, Stubenrauch, CJ, Wu, L |
---|---|
التنسيق: | Journal article |
اللغة: | English |
منشور في: |
Springer
2024
|
مواد مشابهة
-
Convective organization and 3D structure of tropical cloud systems deduced from synergistic A-Train observations and machine learning
حسب: C. J. Stubenrauch, وآخرون
منشور في: (2023-05-01) -
Climate Models Underestimate Dynamic Cloud Feedbacks in the Tropics
حسب: P. G. Hill, وآخرون
منشور في: (2023-08-01) -
Cloud-convection feedback in brown dwarf atmospheres
حسب: Lefevre, M, وآخرون
منشور في: (2022) -
Feedback mechanisms of shallow convective clouds in a warmer climate as demonstrated by changes in buoyancy
حسب: Dagan, G, وآخرون
منشور في: (2018) -
Feedback mechanisms of shallow convective clouds in a warmer climate as demonstrated by changes in buoyancy
حسب: G Dagan, وآخرون
منشور في: (2018-01-01)