On the critical Richardson number in stably stratified turbulence

被引:208
作者
Galperin, Boris [1 ]
Sukoriansky, Semion [2 ]
Anderson, Philip S. [3 ]
机构
[1] Univ S Florida, Coll Marine Sci, St Petersburg, FL 33701 USA
[2] Ben Gurion Univ Negev, Dept Mech Engn, Perlstone Ctr Aeronaut Engn Studies, IL-84105 Beer Sheva, Israel
[3] British Antarctic Survey, Antarctic Climate & Earth Syst Programme, Cambridge CB3 0ET, England
基金
以色列科学基金会;
关键词
turbulence; stable stratification; critical Richardson number; SURFACE-LAYERS; BOUNDARY-LAYER; ROTATING STARS; CLOSURE-MODEL; GRAVITY-WAVES; MIXED-LAYER; SHEAR-LAYER; FLOWS; STABILITY; DIFFUSION;
D O I
10.1002/asl.153
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The critical Richardson number, Ri(c), is used in studies of stably stratified turbulence as a measure of flow laminarization. The accepted range of Ri(c) is between 0.2 and 1. A growing body of experimental and observational data indicates, however, that turbulence survives for Ri >> 1. This result is supported by a new spectral theory of turbulence that accounts for strong anisotropy and waves. The anisotropization results in the enhanced horizontal mixing of both momentum and scalar. Internal wave contribution preserves vertical momentum mixing above its molecular level. In the absence of laminarization, Ri(c) becomes devoid of its conventional meaning. Copyright (C) 2007 Royal Meteorological Society
引用
收藏
页码:65 / 69
页数:5
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