MIXING IN THE EQUATORIAL SURFACE-LAYER AND THERMOCLINE

被引：141

作者：

MOUM, JN

CALDWELL, DR

PAULSON, CA

机构：

来源：

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS | 1989年 / 94卷 / C2期

关键词：

D O I：

10.1029/JC094iC02p02005

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

引用

页码：2005 / 2021

页数：17

共 59 条

[21] GENERATION OF INTERNAL WAVES BY TURBULENCE IN THE MIXED LAYER [J].

KANTHA, LH .

[22]

LARGE WG, 1981, J PHYS OCEANOGR, V11, P324, DOI 10.1175/1520-0485(1981)011<0324:OOMFMI>2.0.CO

[23]

[24] DEEPENING OF A MIXED LAYER IN A STRATIFIED FLUID [J].

LINDEN, PF .

[25]

LUECK RG, 1983, J PHYS OCEANOGR, V13, P1809, DOI 10.1175/1520-0485(1983)013<1809:TDOTCS>2.0.CO

[26]

[27] A LINEAR STRATIFIED OCEAN MODEL OF THE EQUATORIAL UNDERCURRENT [J].

MCCREARY, JP .

PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1981, 298 (1444) :603-635

[28] ON THE STABILITY OF HETEROGENEOUS SHEAR FLOWS [J].

MILES, JW .

[29]

MONIN AS, 1975, STATISTICAL FLUID ME, V2

[30]

MOUM JN, 1986, J PHYS OCEANOGR, V16, P1991, DOI 10.1175/1520-0485(1986)016<1991:DOTPAT>2.0.CO