Radiative Effects of Stratospheric Seasonal Cycles in the Tropical Upper Troposphere and Lower Stratosphere
Water vapor and ozone are powerful radiative constituents in the tropical lower stratosphere, impacting the local heating budget and nonlocally forcing the troposphere below. Their near-tropopause seasonal cycle structures imply associated "radiative seasonal cycles" in heating rates that...
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American Meteorological Society
2017
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| Online Access: | http://hdl.handle.net/1721.1/112934 https://orcid.org/0000-0003-2422-0887 https://orcid.org/0000-0002-2020-7581 |