globalchange  > 气候减缓与适应
DOI: 10.1002/2014GL062421
论文题名:
Extremely long Kelvin-Helmholtz billow trains in the Romanche Fracture Zone
作者: Van Haren H.; Gostiaux L.; Morozov E.; Tarakanov R.
刊名: Geophysical Research Letters
ISSN: 0094-9531
EISSN: 1944-9262
出版年: 2014
卷: 41, 期:23
起始页码: 8445
结束页码: 8451
语种: 英语
英文关键词: Kelvin-Helmholtz billows ; mixing Antarctic Bottom Water ; Romanche Fracture Zone
Scopus关键词: Fracture ; Mixing ; Tides ; Antarctic Bottom Water ; Fracture zone ; High resolution ; Kelvin-Helmholtz billows ; Mid Atlantic Ridge ; Overlying water ; Steady shear flow ; Turbulent mixing ; Shear flow ; fracture zone ; ocean basin ; sensor ; shear flow ; water depth ; water mass ; Atlantic Ocean
英文摘要: In the Atlantic Ocean, the densest water mass Antarctic Bottom Water "AABW" can only cross the Mid-Atlantic Ridge from its southwestern to northeastern basins in limited, because deep, conduits. At the southwestern entrance of one of these, the equatorial Romanche Fracture Zone, AABW crosses a sill at 4550 m depth in a 7 km narrow channel before plunging into the deep. At the sill-slope, the rapidly flowing AABW causes shear-induced turbulent mixing with the overlying water masses. We present an excerpt of 1 Hz sampled, half-yearlong moored observations from 99 high-resolution temperature sensors that demonstrate and quantify the turbulence details. On top of quasi-steady shear flow, an internal tide modulates the mixing. Together, they constitute a means for an extremely long train of >250 consecutive Kelvin-Helmholtz billows in a day that vary between 5 and 100 m in vertical scale. © 2014. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84921567947&doi=10.1002%2f2014GL062421&partnerID=40&md5=07d67b8e59999e925169083ce0e912cf
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/6795
Appears in Collections:气候减缓与适应

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作者单位: NIOZ Royal Netherlands Institute for Sea Research, Den Burg, Netherlands

Recommended Citation:
Van Haren H.,Gostiaux L.,Morozov E.,et al. Extremely long Kelvin-Helmholtz billow trains in the Romanche Fracture Zone[J]. Geophysical Research Letters,2014-01-01,41(23).
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