IOCAS-IR  > 海洋环流与波动重点实验室
Hydraulic control of flow in a multi-passage system connecting two basins
Tan, S.1,2,3,4; Pratt, L. J.1; Voet, G.5; Cusack, J. M.5,6; Helfrich, K. R.1; Alford, M. H.5; Girton, J. B.7; Carter, G. S.8
2022-04-05
发表期刊JOURNAL OF FLUID MECHANICS
ISSN0022-1120
卷号940页码:32
通讯作者Tan, S.(shuwent@ldeo.columbia.edu)
摘要When a fluid stream in a conduit splits in order to pass around an obstruction, it is possible that one branch will be critically controlled while the other remains not so. This is apparently the situation in Pacific Ocean abyssal circulation, where most of the northward flow of Antarctic bottom water passes through the Samoan Passage, where it is hydraulically controlled, while the remainder is diverted around the Manihiki Plateau and is not controlled. These observations raise a number of questions concerning the dynamics necessary to support such a regime in the steady state, the nature of upstream influence and the usefulness of rotating hydraulic theory to predict the partitioning of volume transport between the two paths, which assumes the controlled branch is inviscid. Through the use of a theory for constant potential vorticity flow and accompanying numerical model, we show that a steady-state regime similar to what is observed is dynamically possible provided that sufficient bottom friction is present in the uncontrolled branch. In this case, the upstream influence that typically exists for rotating channel flow is transformed into influence into how the flow is partitioned. As a result, the partitioning of volume flux can still be reasonably well predicted with an inviscid theory that exploits the lack of upstream influence.
关键词hydraulic control ocean circulation shallow water flows
DOI10.1017/jfm.2022.212
收录类别SCI
语种英语
资助项目National Science Foundation[OCE-1029268] ; National Science Foundation[OCE-1029483] ; National Science Foundation[OCE-1657264] ; National Science Foundation[OCE-1657795] ; National Science Foundation[OCE-1657870] ; National Science Foundation[OCE-1658027]
WOS研究方向Mechanics ; Physics
WOS类目Mechanics ; Physics, Fluids & Plasmas
WOS记录号WOS:000778235900001
出版者CAMBRIDGE UNIV PRESS
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被引频次:1[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/178622
专题海洋环流与波动重点实验室
通讯作者Tan, S.
作者单位1.Woods Hole Oceanog Inst, Dept Phys Oceanog, Woods Hole, MA 02543 USA
2.Columbia Univ, Lamont Doherty Earth Observ, New York, NY 10027 USA
3.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Shandong, Peoples R China
4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
5.Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
6.Rutgers State Univ, New Brunswick, NJ 08901 USA
7.Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA
8.Univ Hawaii Manoa, Dept Oceanog, Honolulu, HI 96822 USA
第一作者单位海洋环流与波动重点实验室
通讯作者单位海洋环流与波动重点实验室
推荐引用方式
GB/T 7714
Tan, S.,Pratt, L. J.,Voet, G.,et al. Hydraulic control of flow in a multi-passage system connecting two basins[J]. JOURNAL OF FLUID MECHANICS,2022,940:32.
APA Tan, S..,Pratt, L. J..,Voet, G..,Cusack, J. M..,Helfrich, K. R..,...&Carter, G. S..(2022).Hydraulic control of flow in a multi-passage system connecting two basins.JOURNAL OF FLUID MECHANICS,940,32.
MLA Tan, S.,et al."Hydraulic control of flow in a multi-passage system connecting two basins".JOURNAL OF FLUID MECHANICS 940(2022):32.
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