Clouds, Circulation, and Climate Sensitivity in a Radiative-Convective Equilibrium Channel Model
Tropical cloud and circulation changes are large sources of uncertainty in future climate change. This problem owes partly to the scale separation between large-scale tropical dynamics (~104km) and convective dynamics (~7 km), which generally requires parameterizing convection in models that resolve...
Main Authors: | Cronin, Timothy Wallace (Contributor), Wing, Allison A. (Contributor) |
---|---|
Other Authors: | Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor) |
Format: | Article |
Language: | English |
Published: |
American Geophysical Union (AGU),
2018-09-21T15:36:21Z.
|
Subjects: | |
Online Access: | Get fulltext |
Similar Items
-
Understanding the Extreme Spread in Climate Sensitivity within the Radiative‐Convective Equilibrium Model Intercomparison Project
by: Tobias Becker, et al.
Published: (2020-10-01) -
The climate time scale in the approach to radiative-convective equilibrium
by: Cronin, Timothy W., et al.
Published: (2015) -
Increase in Precipitation Efficiency With Surface Warming in Radiative‐Convective Equilibrium
by: Lutsko, Nicholas J., et al.
Published: (2020) -
Island precipitation enhancement and the diurnal cycle in radiative-convective equilibrium
by: Cronin, Timothy Wallace, et al.
Published: (2015) -
Radiative–convective equilibrium model intercomparison project
by: A. A. Wing, et al.
Published: (2018-03-01)