Vertical structure of warming consistent with an upward shift in the middle and upper troposphere
Warming in climate-change simulations reaches a local maximum in the tropical upper troposphere as expected from moist-adiabatic lapse rates. But the structure of warming varies between models and differs substantially from moist adiabatic in the extratropics. Here, we relate the vertical profile of...
| Main Authors: | , |
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| Other Authors: | |
| Format: | Article |
| Language: | en_US |
| Published: |
American Geophysical Union (AGU)
2014
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| Online Access: | http://hdl.handle.net/1721.1/85599 https://orcid.org/0000-0003-1748-0816 |