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: | English |
| Published: |
American Geophysical Union (AGU),
2014-03-10T20:18:29Z.
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| Subjects: | |
| Online Access: | Get fulltext |