Hydrological Variation at the Southern Margin of the Western Pacific Warm Pool over the past 360 kyrs

Hydrological Variation at the Southern Margin of the Western Pacific Warm Pool over the past 360 kyrs

碩士 === 國立臺灣大學 === 地質科學研究所 === 100 === The Western Pacific Warm Pool (WPWP) plays a key role in the global climate system because it is the greatest warm region of the oceans worldwide and the large heat capacity supplying the latent heat and moisture in global climate changes. By analyzing Mg/Ca rat...

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Main Authors: SHENG-PU CHANG, 張聖菩
Other Authors: Chuan-Chou Shen
Format: Others
Language:en_US
Published: 2012
Online Access:http://ndltd.ncl.edu.tw/handle/29587669694327699951
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spelling ndltd-TW-100NTU051380212015-10-13T21:50:17Z http://ndltd.ncl.edu.tw/handle/29587669694327699951 Hydrological Variation at the Southern Margin of the Western Pacific Warm Pool over the past 360 kyrs 西太平洋暖池南緣過去36萬年來的海表水文變化 SHENG-PU CHANG 張聖菩 碩士 國立臺灣大學 地質科學研究所 100 The Western Pacific Warm Pool (WPWP) plays a key role in the global climate system because it is the greatest warm region of the oceans worldwide and the large heat capacity supplying the latent heat and moisture in global climate changes. By analyzing Mg/Ca ratios of planktonic foraminifer, Globigerinoides ruber white, s.s., (250-300 μm) of a sediment core MD05-2925 (9.344 oS, 151.460 oE, water depth 1661 m) over the past 360 thousand years at the sensitive southern margin of the WPWP (SMWP), the results show five features. (1) WPWP thermal condition is strongly associated with global sea level change. The global climate changes may be triggered by thermal/hydrological conditions of the WPWP. (2) The derived sea surface water Chuan-Chou Shen 沈川洲 2012 學位論文 ; thesis 47 en_US
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language en_US
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description 碩士 === 國立臺灣大學 === 地質科學研究所 === 100 === The Western Pacific Warm Pool (WPWP) plays a key role in the global climate system because it is the greatest warm region of the oceans worldwide and the large heat capacity supplying the latent heat and moisture in global climate changes. By analyzing Mg/Ca ratios of planktonic foraminifer, Globigerinoides ruber white, s.s., (250-300 μm) of a sediment core MD05-2925 (9.344 oS, 151.460 oE, water depth 1661 m) over the past 360 thousand years at the sensitive southern margin of the WPWP (SMWP), the results show five features. (1) WPWP thermal condition is strongly associated with global sea level change. The global climate changes may be triggered by thermal/hydrological conditions of the WPWP. (2) The derived sea surface water
author2 Chuan-Chou Shen
author_facet Chuan-Chou Shen
SHENG-PU CHANG
張聖菩
author SHENG-PU CHANG
張聖菩
spellingShingle SHENG-PU CHANG
張聖菩
Hydrological Variation at the Southern Margin of the Western Pacific Warm Pool over the past 360 kyrs
author_sort SHENG-PU CHANG
title Hydrological Variation at the Southern Margin of the Western Pacific Warm Pool over the past 360 kyrs
title_short Hydrological Variation at the Southern Margin of the Western Pacific Warm Pool over the past 360 kyrs
title_full Hydrological Variation at the Southern Margin of the Western Pacific Warm Pool over the past 360 kyrs
title_fullStr Hydrological Variation at the Southern Margin of the Western Pacific Warm Pool over the past 360 kyrs
title_full_unstemmed Hydrological Variation at the Southern Margin of the Western Pacific Warm Pool over the past 360 kyrs
title_sort hydrological variation at the southern margin of the western pacific warm pool over the past 360 kyrs
publishDate 2012
url http://ndltd.ncl.edu.tw/handle/29587669694327699951
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