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The effect of vertical shear on tropical cyclone intensity change
The effect of vertical shear on tropical cyclone intensity change is ususally explained in terms of "ventilation" where heat and moisture at upper levels are advected away from the low-level circulation, which inhibits development. A simple two-layer diagnostic balance model is used to pro...
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Published in: | Journal of the atmospheric sciences 1996-07, Vol.53 (14), p.2076-2087 |
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Language: | English |
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container_end_page | 2087 |
container_issue | 14 |
container_start_page | 2076 |
container_title | Journal of the atmospheric sciences |
container_volume | 53 |
creator | DEMARIA, M |
description | The effect of vertical shear on tropical cyclone intensity change is ususally explained in terms of "ventilation" where heat and moisture at upper levels are advected away from the low-level circulation, which inhibits development. A simple two-layer diagnostic balance model is used to provide an alternate explanation of the effect of shear. |
doi_str_mv | 10.1175/1520-0469(1996)053<2076:teovso>2.0.co;2 |
format | article |
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ispartof | Journal of the atmospheric sciences, 1996-07, Vol.53 (14), p.2076-2087 |
issn | 0022-4928 1520-0469 |
language | eng |
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source | EZB Electronic Journals Library |
subjects | Atmosphere Cyclones Earth, ocean, space Exact sciences and technology External geophysics Marine Meteorology Science Storms, hurricanes, tornadoes, thunderstorms Tropical cyclones Ventilation |
title | The effect of vertical shear on tropical cyclone intensity change |
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