Internal wave generation in a global baroclinic tide model

被引:263
作者
Simmons, HL [1 ]
Hallberg, RW
Arbic, BK
机构
[1] Univ Alaska Fairbanks, Int Arctic Res Ctr, Fairbanks, AK 99775 USA
[2] Geophys Fluid Dynam Lab, Princeton, NJ 08542 USA
[3] Princeton Univ, Program Atmospher & Ocean Sci, Princeton, NJ 08544 USA
关键词
D O I
10.1016/j.dsr2.2004.09.015
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The energy flux out of barotropic tides and into internal waves ("conversion") is computed using a global domain multi-layer numerical model. The solution is highly baroclinic and reveals a global field of internal waves radiating way from generation sites of rough topography. A small number of sites where intense internal wave generation occurs accounts for most of the globally integrated work done on the barotropic tide and dominates sites such as the Mid-Atlantic ridge. The globally integrated conversion of the M-2 barotropic tide is 891 Gigawatts and the globally integrated rate of working of the ocean by astronomical forcing is 2.94 Terawatts. Both of these estimates are close to accepted values derived from independent methods. Regional estimates of conversion are also similar to previous inferences, lending additional confidence that the solution has captured the essential physics of low-mode internal wave generation and that numerical prediction of conversion has skill in regions where no previous estimates are available. (C) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:3043 / 3068
页数:26
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