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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
Main Author: DEMARIA, M
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Language:English
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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
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ispartof Journal of the atmospheric sciences, 1996-07, Vol.53 (14), p.2076-2087
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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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