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

[1] ARMI L, 1983, J PHYS OCEANOGR, V13, P828, DOI 10.1175/1520-0485(1983)013<0828:FVOAPO>2.0.CO
[2] 2
[3] Baumgartner A., 1975, WORLD WATER BALANCE
[4] DANTZLER HL, 1977, J PHYS OCEANOGR, V7, P512, DOI 10.1175/1520-0485(1977)007<0512:PEMITT>2.0.CO
[5] 2
[6] Defant A., 1936, WISS ERGEBN DTSCH AT, V6, P289
[7] EMERY WJ, 1982, MEAN TEMPERATURE SAL
[8] VERTICAL EDDY DIFFUSIVITY IN THE OCEAN INTERIOR
GARGETT, AE
[J]. JOURNAL OF MARINE RESEARCH, 1984, 42 (02) : 359 - 393
[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
LAMBERT, RB
STURGES, W
[J]. DEEP-SEA RESEARCH, 1977, 24 (03): : 211 - 222