THE RELATIVE CONTRIBUTIONS OF ADVECTION AND ISOPYCNAL AND DIAPYCNAL MIXING BELOW THE SUB-TROPICAL SALINITY MAXIMUM

被引：28

作者：

BAUER, E ^{[1
]}

SIEDLER, G ^{[1
]}

机构：

[1] INST MEERESKUNDE,D-2300 KIEL,FED REP GER

来源：

DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS | 1988年 / 35卷 / 05期

关键词：

D O I：

10.1016/0198-0149(88)90032-5

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

引用

页码：811 / 837

页数：27

共 32 条

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[5]

[6]

Defant A., 1936, WISS ERGEBN DTSCH AT, V6, P289

[7]

EMERY WJ, 1982, MEAN TEMPERATURE SAL

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[9]

Gill A. E., 1982, ATMOSPHERE OCEAN DYN, DOI DOI 10.1016/S0074-6142(08)60034-0

[10] THERMOHALINE STAIRCASE AND VERTICAL MIXING IN THERMOCLINE [J].

LAMBERT, RB ;

STURGES, W .

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