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Effects of Gap-Wind-Induced Vorticity, the Monsoon Trough, and the ITCZ on Tropical Cyclogenesis

Title: The Effects of Gap-Wind-Induced Vorticity, the Monsoon Trough, and the ITCZ on Tropical Cyclogenesis.
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Name(s): Holbach, Heather, author
Bourassa, Mark, professor directing thesis
Hart, Robert, committee member
Liu, Guosheng, committee member
Powell, Mark, committee member
Department of Earth, Ocean and Atmospheric Sciences, degree granting department
Florida State University, degree granting institution
Type of Resource: text
Genre: text
Issuance: monographic
Date Issued: 2012
Publisher: Florida State University
Place of Publication: Tallahassee, Florida
Physical Form: computer
Physical Form: online resource
Extent: 1 online resource
Language(s): English
Abstract/Description: Tropical cyclogenesis in the eastern North Pacific (EPAC) basin is related to gap-wind-induced vorticity, the monsoon trough, and the intertropical convergence zone (ITCZ). There are several gaps in the Central American Mountains, on the eastern edge of the EPAC basin, through which wind can be funneled to generate surface wind jets (gap winds). This study focuses on gap winds that occur over the Gulf of Papagayo and the Gulf of Tehuantepec. QuikSCAT (QSCAT) 10 m equivalent neutral winds are used to identify gap wind events that occur during May through November of 2002-2008. Dvorak fix locations, GridSAT IR data, and National Hurricane Center Tropical Cyclone (TC) Reports are used to track the disturbances that occurred during the study period. Surface vorticity is tracked using the QSCAT winds and the contribution of vorticity from the gap winds to the development of each disturbance is categorized as small, medium, or large. Cross-calibrated multiplatform (CCMP) surface wind data are used to verify the tracking of QSCAT computed vorticity and to identify when the monsoon trough and the ITCZ are present. It is found that gap winds are present over the Gulf of Papagayo and the Gulf of Tehuantepec for more than 50% of the QSCAT coverage days and that these gap winds appear to contribute to the development of disturbances in the EPAC. Considerably more TCs form when the monsoon trough is present versus the ITCZ and the majority of the contributions from the gap winds also occur when the monsoon trough is present.
Identifier: FSU_migr_etd-4913 (IID)
Submitted Note: A Thesis submitted to the Department of Earth, Ocean and Atmospheric Science in partial fulfillment of the requirements for the degree of Master of Science.
Degree Awarded: Summer Semester, 2012.
Date of Defense: June 29, 2012.
Keywords: Gap winds, ITCZ, Monsoon Trough, Papagayo, Tehuantepec, Tropical cyclogenesis
Bibliography Note: Includes bibliographical references.
Advisory Committee: Mark Bourassa, Professor Directing Thesis; Robert Hart, Committee Member; Guosheng Liu, Committee Member; Mark Powell, Committee Member.
Subject(s): Earth sciences
Oceanography
Atmospheric sciences
Geophysics
Persistent Link to This Record: http://purl.flvc.org/fsu/fd/FSU_migr_etd-4913
Owner Institution: FSU

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Holbach, H. (2012). The Effects of Gap-Wind-Induced Vorticity, the Monsoon Trough, and the ITCZ on Tropical Cyclogenesis. Retrieved from http://purl.flvc.org/fsu/fd/FSU_migr_etd-4913