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The Flow Separations in the Taiwan S...

Liao, Enhui.

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The Flow Separations in the Taiwan Strait and Ocean Responses to the "Hiatus" of the Global Mean Surface Temperature.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	The Flow Separations in the Taiwan Strait and Ocean Responses to the "Hiatus" of the Global Mean Surface Temperature./
作者:	Liao, Enhui.
出版者:	Ann Arbor : ProQuest Dissertations & Theses, : 2017,
面頁冊數:	151 p.
附註:	Source: Dissertation Abstracts International, Volume: 79-08(E), Section: B.
Contained By:	Dissertation Abstracts International79-08B(E).
標題:	Physical oceanography. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10640075
ISBN:	9780355758849

The Flow Separations in the Taiwan Strait and Ocean Responses to the "Hiatus" of the Global Mean Surface Temperature.
Liao, Enhui.

The Flow Separations in the Taiwan Strait and Ocean Responses to the "Hiatus" of the Global Mean Surface Temperature. - Ann Arbor : ProQuest Dissertations & Theses, 2017 - 151 p.

Source: Dissertation Abstracts International, Volume: 79-08(E), Section: B.

Thesis (Ph.D.)--University of Delaware, 2017.

Coastlines are fundamental to humans for habitation, commerce, and natural resources. Many coastal ecosystem disasters, caused by extreme sea surface temperature (SST), were reported when the global climate shifted from global warming to global surface warming hiatus between 1998 and 2013. The 2008 cold event in the Taiwan Strait (northwestern Pacific) is one of these disasters. In studying the behind dynamical mechanism of the cold event, four topics were raised in sequence and consisted of my thesis. Two off-shore flows are identified and investigated through observed and model (ROMS) results. In order to better understand this cold event within global context, the global coastal responses and heat redistribution in the Indian Ocean are then studied using satellite data and a global climate model (CESM).

ISBN: 9780355758849Subjects--Topical Terms:

3168433
Physical oceanography.

The Flow Separations in the Taiwan Strait and Ocean Responses to the "Hiatus" of the Global Mean Surface Temperature.
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520 $a Analysis of the vorticity balance shows that the off-shore flow in the southern strait is a result of negative bottom stress curl that is triggered by the positive vorticity over a gentle slope over the bank. The other off-shore flow in the northern strait often makes a U-turn to join the northward-flowing Taiwan wam current. In early 2008, I found the strong local wind stress plus an additional remote forcing (Coastal Kelvin Wave) moved the separated cold southward to the Penghu Island, inducing the cold event. The study on the global coastal SST from 1982 to 2013 revealed a significant cooling trend in the low and mid latitudes (31.4% of the global coastlines) after 1998, while 17.9% of the global coastlines changed from a cooling trend to a warming trend concurrently. These coastal SST changes are larger than the changes of the global mean and open ocean, resulting in a fast increase of extremely hot/cold days, and thus extremely hot/cold events. The study of heat transport in the Indian Ocean discloses a different pathway that the anomalous heat moves southward instead of westward caused by a strengthened southward transport and a weakened south equatorial current. This induces a striking heat build-up in the middle latitude of South Indian Ocean, contributes to the Southern Ocean warming, and intensifies heat hemisphere asymmetry.
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