中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Estimation of the Ventilation Transit Time Distribution at the Yap-Mariana Junction Using Ar-39, Kr-85 and C-14 Tracers

文献类型:期刊论文

作者Gu, Ji-Qiang3; Jiang, Wei3; Tong, Amin L.3; Yang, Guo-Min3; Dong, Xi-Ze3; Ritterbusch, Florian3; Wang, Fan1,2; Wang, Jianing1,2
刊名JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
出版日期2022-07-01
卷号127期号:7页码:12
ISSN号2169-9275
关键词transit time distribution atom trap trace analysis
DOI10.1029/2022JC018417
通讯作者Jiang, Wei(wjiang1@ustc.edu.cn)
英文摘要We report on a multi-tracer study at the Yap-Mariana Junction in the western Pacific using three tracers-Kr-85, Ar-39, and C-14-with different half-lives and source functions to the oceans. The vertical profiles of Kr-85 and Ar-39 are measured using the state-of-the-art Atom Trap Trace Analysis method. This method allows analysis of Kr-85 and Ar-39 isotopes with samples collected in regular Niskin bottles. Combined with the calculated natural C-14 data, we infer the ventilation transit-time distribution (TTD) at the Yap-Mariana Junction. The mean ages of the seawater below the thermocline at the Yap-Mariana Junction are over 1,000 years. Moreover earlier Ar-39 and natural C-14 data collected in other parts of the Pacific are used to infer the local TTDs and compared with the one at the Yap-Mariana Junction. The age spectra of the Pacific bottom waters show progressive changes and increasing tails of the old water along the route from south to north. The dominance of the North Pacific Deep Water (NPDW) in the North Pacific and the effect of mixing between old water masses and younger ones at the Yap-Mariana Junction are reflected from the different shapes of the TTDs at these locations. The TTD shows the oldest water exists at about 2,000 m depth in the North Pacific. The western Pacific shows the highest degree of mixing at 1,000 m depth, while the southern Pacific has the highest degree of mixing close to the bottom.
资助项目National Key Research and Development Program of China[2016YFA0302200] ; National Natural Science Foundation of China, NSFC[41727901] ; National Natural Science Foundation of China, NSFC[41861224007] ; National Natural Science Foundation of China, NSFC[41961144027] ; Anhui Initiative in Quantum Information Technologies[AHY110000] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB21010200] ; NSFC[91958204] ; NSFC[42090040]
WOS研究方向Oceanography
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:000817909300001
源URL[http://ir.qdio.ac.cn/handle/337002/179646]  
专题海洋研究所_海洋环流与波动重点实验室
海洋研究所_深海极端环境与生命过程研究中心
通讯作者Jiang, Wei
作者单位1.Chinese Acad Sci, Ctr Deepsea Res, Inst Oceanol, Qingdao, Peoples R China
2.Chinese Acad Sci, Key Lab Ocean Circulat & Waves, Inst Oceanol, Qingdao, Peoples R China
3.Univ Sci & Technol China, Sch Phys Sci, Hefei, Peoples R China
推荐引用方式
GB/T 7714
Gu, Ji-Qiang,Jiang, Wei,Tong, Amin L.,et al. Estimation of the Ventilation Transit Time Distribution at the Yap-Mariana Junction Using Ar-39, Kr-85 and C-14 Tracers[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2022,127(7):12.
APA Gu, Ji-Qiang.,Jiang, Wei.,Tong, Amin L..,Yang, Guo-Min.,Dong, Xi-Ze.,...&Wang, Jianing.(2022).Estimation of the Ventilation Transit Time Distribution at the Yap-Mariana Junction Using Ar-39, Kr-85 and C-14 Tracers.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,127(7),12.
MLA Gu, Ji-Qiang,et al."Estimation of the Ventilation Transit Time Distribution at the Yap-Mariana Junction Using Ar-39, Kr-85 and C-14 Tracers".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 127.7(2022):12.

入库方式: OAI收割

来源:海洋研究所

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