THE GULF STREAM AS AN INERTIAL BOUNDARY LAYER

被引:156
作者
CHARNEY, JG
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D O I
10.1073/pnas.41.10.731
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
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页码:731 / 740
页数:10
相关论文
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[1]  
CHARNEY JG, 1955, UNPUB J MARINE RES, V14
[2]  
FOFONOFF NP, 1954, J MARINE RES, V2, P254
[3]  
ISELIN CO, 1950, J MARINE RES, V7, P317
[4]  
ISELIN CO, 1940, PAPERS PHYS OCEANOG, V8
[5]  
ISELIN COD, 1936, PAPERS PHYS OCEANOG, V4
[6]  
MUNK WH, 1950, J METEOROL, V7, P79
[7]   Relation between variations in the intensity of the zonal circulation of the atmosphere and the displacements of the semipermanent centers of action [J].
Rossby, CG .
JOURNAL OF MARINE RESEARCH, 1939, 2 (01) :38-55
[8]  
Stommel H., 1948, T AM GEOPHYS UNION, V29, P202, DOI [10.1029/TR029i002p00202, DOI 10.1029/TR029I002P00202]
[9]  
Sverdrup H. U., 1942, OCEANS