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DOI10.1029/2020GL087266
Using Excess 3He to Estimate Southern Ocean Upwelling Time Scales
Jenkins W.J.
发表日期2020
ISSN 0094-8276
卷号47期号:15
英文摘要Using a recently compiled global marine data set of dissolved helium isotopes and helium and neon concentrations, we make an estimate of the inventory of hydrothermal 3He in the Southern Ocean to be 4.9 ± 0.6 × 104 moles. Under the assumption that the bulk of the hydrothermally sourced 3He is upwelled there, we use recent estimates of the global hydrothermal 3He flux to determine an e-folding residence time of 99 ± 18 years, depending on assumptions of water mass and upwelling boundaries. Our estimate is within the broad range of values obtained from recent Southern Ocean circulation models. ©2020. American Geophysical Union. All Rights Reserved.
英文关键词Helium; E-folding; Global marines; Helium isotopes; Hydrothermally; Residence time; Southern ocean; Time-scales; Water mass; Oceanography; circulation modeling; concentration (composition); data set; helium; hydrothermal circulation; neon; timescale; upwelling; water mass; Southern Ocean
语种英语
来源期刊Geophysical Research Letters
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/170040
作者单位Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA, United States
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Jenkins W.J.. Using Excess 3He to Estimate Southern Ocean Upwelling Time Scales[J],2020,47(15).
APA Jenkins W.J..(2020).Using Excess 3He to Estimate Southern Ocean Upwelling Time Scales.Geophysical Research Letters,47(15).
MLA Jenkins W.J.."Using Excess 3He to Estimate Southern Ocean Upwelling Time Scales".Geophysical Research Letters 47.15(2020).
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