globalchange  > 气候减缓与适应
DOI: 10.1002/grl.50510
论文题名:
Tidal dissipation in the early Eocene and implications for ocean mixing
作者: Green J.A.M.; Huber M.
刊名: Geophysical Research Letters
ISSN: 0094-8960
EISSN: 1944-8691
出版年: 2013
卷: 40, 期:11
起始页码: 2707
结束页码: 2713
语种: 英语
英文关键词: early Eocene ; Meridional Overturning Circulation ; ocean mixing ; tides ; Vertical diffusivity
Scopus关键词: Early Eocene ; Evolution history ; Meridional overturning circulations ; Ocean mixing ; Tidal dissipation ; Vertical diffusivity ; Vertical stratification ; Warm temperatures ; Mixing ; Tides ; Oceanography ; abyssal circulation ; diffusivity ; dissipation ; Eocene ; meridional circulation ; mixing ; paleoclimate ; tidal modeling ; Pacific Ocean ; Pacific Ocean (Southwest)
英文摘要: The tidally driven vertical diffusivity in the abyssal ocean during the early Eocene (55 Ma) is investigated using an established tidal model. A weak tide is predicted in the Eocene ocean, except in the Pacific. Consequently, the integrated global tidal dissipation rate is a mere 1.44TW, of which 40% dissipate in the Pacific. However, due to a stronger abyssal vertical stratification the predicted Eocene vertical diffusivities are consistently larger than at present. The results support the hypothesis that altered tidal dissipation may play a role in explaining the maintenance of past climate regimes, especially the anomalously warm temperatures in the southwest Pacific in the Eocene, and the low dissipation rates may be important for lunar evolution history. © 2013 American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84879603472&doi=10.1002%2fgrl.50510&partnerID=40&md5=a5becb2660a23a66f939acaf99efd529
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/6224
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作者单位: School of Ocean Sciences, Bangor University, Menai Bridge, LL59 5AB, United Kingdom

Recommended Citation:
Green J.A.M.,Huber M.. Tidal dissipation in the early Eocene and implications for ocean mixing[J]. Geophysical Research Letters,2013-01-01,40(11).
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