Antarctic Radiative and Temperature Responses to a Doubling of CO 2
Author:
Affiliation:
1. Department of Earth, Atmosphere and Planetary Sciences Massachusetts Institute of Technology Cambridge MA USA
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL093676
Reference28 articles.
1. Large Increase in Incident Shortwave Radiation due to the Ozone Hole Offset by High Climatological Albedo over Antarctica
2. Analytic radiative‐advective equilibrium as a model for high‐latitude climate
3. Climate Response to Negative Greenhouse Gas Radiative Forcing in Polar Winter
4. On the warming in the tropical upper troposphere: Models versus observations
5. Why logarithmic? A note on the dependence of radiative forcing on gas concentration
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1. Infrared Radiative Effects of Increasing CO2 and CH4 on the Atmosphere in Antarctica Compared to the Arctic;Geophysical Research Letters;2024-01-19
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3. The Global Patterns of Instantaneous CO2 Forcing at the Top of the Atmosphere and the Surface;Journal of Climate;2023-09-15
4. The global patterns of instantaneous CO2 forcing at the top-of-atmosphere and surface;2022-09-23
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