Convective mixing near the tropical tropopause: Insights from seasonal variations
Sherwood and Dessler present an explicit model of the interaction between overshooting convection and large-scale processes. They emphasized the importance of a tropical tropopause layer between about 14 and 19 km, rather than a specific tropopause or other surface, as the true mediator or exchange...
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| Veröffentlicht in: | Journal of the atmospheric sciences 2003-11, Vol.60 (21), p.2674-2685 |
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| container_end_page | 2685 |
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| container_issue | 21 |
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| container_title | Journal of the atmospheric sciences |
| container_volume | 60 |
| creator | SHERWOOD, Steven C DESSLER, Andrew E |
| description | Sherwood and Dessler present an explicit model of the interaction between overshooting convection and large-scale processes. They emphasized the importance of a tropical tropopause layer between about 14 and 19 km, rather than a specific tropopause or other surface, as the true mediator or exchange between the troposphere and stratosphere. |
| doi_str_mv | 10.1175/1520-0469(2003)060<2674:cmnttt>2.0.co;2 |
| format | Article |
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| source | American Meteorological Society; EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection |
| subjects | Atmosphere Atmospheric pressure Boundary layers Carbon dioxide Climate models Convection Convective mixing Convective transport Cycles Dehydration Earth, ocean, space Exact sciences and technology External geophysics Lower stratosphere Meteorology Modelling Phase lag Physics Physics of the high neutral atmosphere Planetary boundary layer Seasonal variation Seasonal variations Stratosphere Temperature Thickness Tides, waves, convection, winds, turbulence Tracers Tropical tropopause Tropopause Tropopause temperatures Troposphere Upper troposphere Vertical velocities Water in the atmosphere (humidity, clouds, evaporation, precipitation) Water vapor Water vapour |
| title | Convective mixing near the tropical tropopause: Insights from seasonal variations |
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