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Air-Sea Interactions and Ocean Dynam...

Burns, Jessica Maureen.

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Air-Sea Interactions and Ocean Dynamics in the Southwest Tropical Indian Ocean.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Air-Sea Interactions and Ocean Dynamics in the Southwest Tropical Indian Ocean./
作者:	Burns, Jessica Maureen.
出版者:	Ann Arbor : ProQuest Dissertations & Theses, : 2017,
面頁冊數:	82 p.
附註:	Source: Masters Abstracts International, Volume: 56-05.
Contained By:	Masters Abstracts International56-05(E).
標題:	Physical oceanography. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10258246
ISBN:	9780355071443

Air-Sea Interactions and Ocean Dynamics in the Southwest Tropical Indian Ocean.
Burns, Jessica Maureen.

Air-Sea Interactions and Ocean Dynamics in the Southwest Tropical Indian Ocean. - Ann Arbor : ProQuest Dissertations & Theses, 2017 - 82 p.

Source: Masters Abstracts International, Volume: 56-05.

Thesis (M.S.)--University of South Carolina, 2017.

The Southwest Tropical Indian Ocean (SWTIO) features a unique, seasonal upward lift of the thermocline, which is known as the Seychelles-Chagos Thermocline Ridge (SCTR; 55°E-65°E, 5°S-12°S). It is known that a high correlation exists between the depth of the thermocline and sea surface temperature (SST; a key ingredient for tropical cyclogenesis). With a particular focus on 2012/2013, this study reveals the dynamic properties of the SCTR that play an important role in the modulation of tropical cyclones in the SWTIO. Phenomena including Indian Ocean Dipole (IOD) and El Nino Southern Oscillation (ENSO) are also well correlated to cyclogenesis through changes in the thermocline of the SCTR. More tropical cyclones form over the SWTIO when the thermocline is deeper, which has a positive relation to the arrival of downwelling Rossby waves originating in the southeast tropical Indian Ocean due to the anomalous effects of IOD.

ISBN: 9780355071443Subjects--Topical Terms:

3168433
Physical oceanography.

Air-Sea Interactions and Ocean Dynamics in the Southwest Tropical Indian Ocean.
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520 $a The Southwest Tropical Indian Ocean (SWTIO) features a unique, seasonal upward lift of the thermocline, which is known as the Seychelles-Chagos Thermocline Ridge (SCTR; 55°E-65°E, 5°S-12°S). It is known that a high correlation exists between the depth of the thermocline and sea surface temperature (SST; a key ingredient for tropical cyclogenesis). With a particular focus on 2012/2013, this study reveals the dynamic properties of the SCTR that play an important role in the modulation of tropical cyclones in the SWTIO. Phenomena including Indian Ocean Dipole (IOD) and El Nino Southern Oscillation (ENSO) are also well correlated to cyclogenesis through changes in the thermocline of the SCTR. More tropical cyclones form over the SWTIO when the thermocline is deeper, which has a positive relation to the arrival of downwelling Rossby waves originating in the southeast tropical Indian Ocean due to the anomalous effects of IOD.
520 $a In addition to influencing cyclogeneis over the SCTR region, remote processes such as IOD and ENSO are also the primary drivers of the SCTR interannual variability with respect to both ocean temperature and salinity. Thus, this study also explores how temperature and salinity with depth, as well as at the surface, in the SCTR change with the climatic events in a given year. Although ENSO is known to have a stronger impact on SST south of the SCTR (10°S-15°S), this study reveals the stronger impact of ENSO on sea surface salinity (SSS) in the SCTR.
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