Isentropic Descent beneath the Saharan Air Layer and its Impact on Tropical Cyclogensis

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dc.contributor.advisor Dr. Lian Xie, Committee Member en_US
dc.contributor.advisor Dr. Anantha Aiyyer, Committee Member en_US
dc.contributor.advisor Dr. Fredrick Semazzi, Committee Chair en_US
dc.contributor.author Diaz, Michael en_US
dc.date.accessioned 2010-04-02T18:05:17Z
dc.date.available 2010-04-02T18:05:17Z
dc.date.issued 2009-11-24 en_US
dc.identifier.other etd-11032009-142132 en_US
dc.identifier.uri http://www.lib.ncsu.edu/resolver/1840.16/1581
dc.description.abstract We investigate the driving mechanism behind strong climatological isentropic descent in the eastern Atlantic and how it affects tropical cyclogenesis from African Easterly Waves (AEW). Our results suggest that this isentropic descent is forced by the warm thermal structure associated with the Saharan Air Layer (SAL) combined with northerly flow on the eastern flank of the Azores high. Since this northerly flow travels from the drier middle troposphere at higher latitudes to the lower troposphere at lower latitudes, it provides a nearly continuous source of dry air off the West African coast. Thus, AEWs traveling south of the SAL often ingest dry air from the middle latitudes into their circulation. Being dry, this air mass may suppress the moist convection required for tropical cyclogenesis. Although this process is intimately linked with the SAL, the air mass involved is distinctly different; it originates from the middle latitudes and travels beneath the SAL. In contrast, previous research emphasizes the negatives impact of the SAL itself on tropical cyclogenesis and concentrates primarily on how strong vertical wind shear, dry mid-level air, and high static stability suppress tropical cyclone convection. In this study, we use the Global Forecast System (GFS) analyses from 2000 to 2008 to perform a back trajectory analysis of air within 191 AEW cases to determine dominant air mass source regions. We ﬠnd that AEWs contain a large fraction of low level air mass which has undergone isentropic descent along the African coast. Our results suggest that AEWs containing larger amounts of this air mass tend to have weaker convection and a lower probability of tropical cyclogenesis. We then investigate the role of sea surface temperature along the northwest African coast north of where AEWs track in moistening the dry air from isentropic descent and thus counteracting its inhibiting impact on convection and tropical cyclogenesis. Based on a series of numerical modeling case studies, we ﬠnd that warming (cooling) SST north of 15◦ N along the African coast increases (decreases) the probability that an AEW will become a tropical cyclone. en_US
dc.rights I hereby certify that, if appropriate, I have obtained and attached hereto a written permission statement from the owner(s) of each third party copyrighted matter to be included in my thesis, dis sertation, or project report, allowing distribution as specified below. I certify that the version I submitted is the same as that approved by my advisory committee. I hereby grant to NC State University or its agents the non-exclusive license to archive and make accessible, under the conditions specified below, my thesis, dissertation, or project report in whole or in part in all forms of media, now or hereafter known. I retain all other ownership rights to the copyright of the thesis, dissertation or project report. I also retain the right to use in future works (such as articles or books) all or part of this thesis, dissertation, or project report. en_US
dc.subject Saharan Air Layer en_US
dc.subject African Easterly Wave en_US
dc.subject tropical cyclone en_US
dc.title Isentropic Descent beneath the Saharan Air Layer and its Impact on Tropical Cyclogensis en_US
dc.degree.name MS en_US
dc.degree.level thesis en_US
dc.degree.discipline Marine, Earth and Atmospheric Sciences en_US


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