Midlevel Ventilation's Constraint on Tropical Cyclone Intensity
Midlevel ventilation, or the flux of low-entropy air into the inner core of a tropical cyclone (TC), is a hypothesized mechanism by which environmental vertical wind shear can constrain a tropical cyclone’s intensity. An idealized framework based on steadiness, axisymmetry, and slantwise neutrality...
| Main Authors: | , |
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| Format: | Article |
| Language: | en_US |
| Published: |
American Meteorological Society
2011
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| Online Access: | http://hdl.handle.net/1721.1/62577 https://orcid.org/0000-0002-2066-2082 |