Correlation between present-day model simulation of Arctic cloud radiative forcing and sea ice consistent with positive winter convective cloud feedback
A positive feedback on winter sea-ice loss, based on warming due to radiative forcing caused by the onset of convective clouds in response to sea-ice loss, has recently been proposed. This feedback has thus far been investigated using a hierarchy of climate models in high CO2 scenarios. This paper e...
Main Authors: | Benjamin D. Leibowicz, Dorian S. Abbot, Kerry Emanuel, Eli Tziperman |
---|---|
Format: | Article |
Language: | English |
Published: |
American Geophysical Union (AGU)
2012-07-01
|
Series: | Journal of Advances in Modeling Earth Systems |
Subjects: | |
Online Access: | http://www.agu.org/journals/ms/ms1207/2012MS000153/ |
Similar Items
-
Correlation between present-day model simulation of Arctic cloud radiative forcing and sea ice consistent with positive winter convective cloud feedback
by: Emanuel, Kerry Andrew, et al.
Published: (2012) -
Recent changes in winter Arctic clouds and their relationships with sea ice and atmospheric conditions
by: Sang-Yoon Jun, et al.
Published: (2016-03-01) -
Explicitly Resolved Cloud Feedbacks in the Radiative‐Convective Equilibrium Model Intercomparison Project
by: C. L. Stauffer, et al.
Published: (2023-11-01) -
Feedback mechanisms of shallow convective clouds in a warmer climate as demonstrated by changes in buoyancy
by: G Dagan, et al.
Published: (2018-01-01) -
Underestimated marine stratocumulus cloud feedback associated with overly active deep convection in models
by: N Hirota, et al.
Published: (2021-01-01)