GENERATION OF OCEANIC TURBULENCE

被引：0
|
作者：
MONIN, AS [1 ]
机构：
[1] ACAD SCI USSR,INST OCEANOL,MOSCOW V-71,USSR
来源：
IZVESTIYA AKADEMII NAUK SSSR FIZIKA ATMOSFERY I OKEANA | 1977年 / 13卷 / 11期
关键词：
FLOW OF FLUIDS - Turbulent;
D O I：
暂无
中图分类号：
P4 [大气科学（气象学）];
学科分类号：
0706 ; 070601 ;
摘要：
An estimate is made of the conditions and the effectiveness of the generation of oceanic turbulence as a result of instability of the velocity gradients in drift flows; large-scale stratified geostrophic flows; and mesoscale unsteady and Ekman bottom flows. In addition, a study is made of the breaking of surface waves, the instability of internal waves, and convection in layers with unstable density stratification.
引用
收藏
页码：1159 / 1168
页数：10
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