Date of Award

1-1-2017

Language

English

Document Type

Master's Thesis

Degree Name

Master of Science (MS)

College/School/Department

Department of Atmospheric and Environmental Sciences

Content Description

1 online resource (ii, viii, 55, pages) : illustrations (some color), color maps.

Dissertation/Thesis Chair

John Molinari

Committee Members

Robert G. Fovell

Keywords

G-IV, Observations, Tropical Cyclones, Turbulence, Atmospheric turbulence, Cyclones, Cirrus clouds

Subject Categories

Atmospheric Sciences | Meteorology

Abstract

Turbulence in the cirrus canopy of tropical cyclones (TCs) can give an indication about the physical processes that occur in this expansive cloud deck. The low stability and/or large shear that likely coincides with turbulent layers can be produced by radiative forcing, convective forcing, and sublimation of frozen precipitation from the cirrus canopy. As a result, turbulence in the cirrus canopy can give an indication about the impact of various physical processes in tropical cyclones.

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