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Warming at the Agulhas Region During the Global Surface Warming Acceleration and Slow-Down.

紀錄類型:	書目-語言資料,手稿 : Monograph/item
正題名/作者:	Warming at the Agulhas Region During the Global Surface Warming Acceleration and Slow-Down./
作者:	Han, Lu.
面頁冊數:	1 online resource (91 pages)
附註:	Source: Masters Abstracts International, Volume: 57-02.
標題:	Physical oceanography. -
電子資源:	click for full text (PQDT)
ISBN:	9780355467574

Warming at the Agulhas Region During the Global Surface Warming Acceleration and Slow-Down.
Han, Lu.

Warming at the Agulhas Region During the Global Surface Warming Acceleration and Slow-Down. - 1 online resource (91 pages)

Source: Masters Abstracts International, Volume: 57-02.

Thesis (M.S.)--University of Delaware, 2017.

Includes bibliographical references

This study investigates the interannual to decadal ocean heat content evolution of the upper 700m in the last three decades at the Agulhas region and emphases on exploring its difference between the global surface warming acceleration and slowdown periods. The Agulhas region is a stagnation point of three circulation systems, the South Atlantic Ocean subtropical gyre, the Indian Ocean subtropical gyre, and the Subtropical Front of the Antarctic Circumpolar Current in the Southern Ocean, and it's the linkage between two ocean basins, the Indian Ocean and the Atlantic Ocean. At this region, the ocean never stops or slows its warming even during the global surface warming slowdown. Besides the warming surface, the deeper layer (200-700m) gains more heat primarily as a result of the deepening isopycnals (heaving), possibly induced by the saltier upper layer water, also with a relatively small contribution of the changes along the isopycnals (spice). The most pronounced isopycnal sinking locates at the Return Current and the neighboring Subtropical Front region, while the isopycnals shoal at the upper layer of the Agulhas Current. Due to the altered wind pattern at the Indian Ocean and Southern Ocean, less heat comes along the Agulhas Current during the slowdown period, and the broadening Return Current moves the warm and saline subtropical water southward, which is subducted into the deeper layer by the reclining isopycnals.

Electronic reproduction.
Ann Arbor, Mich. :
ProQuest,
2018

Mode of access: World Wide Web

ISBN: 9780355467574Subjects--Topical Terms:

1178843
Physical oceanography.
Index Terms--Genre/Form:

554714
Electronic books.

Warming at the Agulhas Region During the Global Surface Warming Acceleration and Slow-Down.
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245 1 0 $a Warming at the Agulhas Region During the Global Surface Warming Acceleration and Slow-Down.
264 0 $c 2017
300 $a 1 online resource (91 pages)
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500 $a Source: Masters Abstracts International, Volume: 57-02.
500 $a Adviser: Xiaohai Yan.
502 $a Thesis (M.S.)--University of Delaware, 2017.
504 $a Includes bibliographical references
520 $a This study investigates the interannual to decadal ocean heat content evolution of the upper 700m in the last three decades at the Agulhas region and emphases on exploring its difference between the global surface warming acceleration and slowdown periods. The Agulhas region is a stagnation point of three circulation systems, the South Atlantic Ocean subtropical gyre, the Indian Ocean subtropical gyre, and the Subtropical Front of the Antarctic Circumpolar Current in the Southern Ocean, and it's the linkage between two ocean basins, the Indian Ocean and the Atlantic Ocean. At this region, the ocean never stops or slows its warming even during the global surface warming slowdown. Besides the warming surface, the deeper layer (200-700m) gains more heat primarily as a result of the deepening isopycnals (heaving), possibly induced by the saltier upper layer water, also with a relatively small contribution of the changes along the isopycnals (spice). The most pronounced isopycnal sinking locates at the Return Current and the neighboring Subtropical Front region, while the isopycnals shoal at the upper layer of the Agulhas Current. Due to the altered wind pattern at the Indian Ocean and Southern Ocean, less heat comes along the Agulhas Current during the slowdown period, and the broadening Return Current moves the warm and saline subtropical water southward, which is subducted into the deeper layer by the reclining isopycnals.
533 $a Electronic reproduction. $b Ann Arbor, Mich. : $c ProQuest, $d 2018
538 $a Mode of access: World Wide Web
650 4 $a Physical oceanography. $3 1178843
655 7 $a Electronic books. $2 local $3 554714
690 $a 0415
710 2 $a ProQuest Information and Learning Co. $3 1178819
710 2 $a University of Delaware. $b Marine Studies. $3 1185909
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=10599503 $z click for full text (PQDT)