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Volumn 26, Issue 11, 1996, Pages 2525-2528

Effect of a constant, zonal wind on wind-driven ocean circulation

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EID: 0000208108     PISSN: 00223670     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0485(1996)026<2525:EOACZW>2.0.CO;2     Document Type: Article
Times cited : (5)

References (5)
  • 1
    • 84958427562 scopus 로고
    • An overlooked aspect of the wind-driven ocean circulation
    • Pedlosky, J., 1968: An overlooked aspect of the wind-driven ocean circulation. J. Fluid Mech., 32, 809-821.
    • (1968) J. Fluid Mech. , vol.32 , pp. 809-821
    • Pedlosky, J.1
  • 3
    • 84981751932 scopus 로고
    • The western intensification of wind-driven ocean currents
    • Stommel, H., 1948: The western intensification of wind-driven ocean currents. Trans. Amer. Geophys. Union, 29, 202-210.
    • (1948) Trans. Amer. Geophys. Union , vol.29 , pp. 202-210
    • Stommel, H.1
  • 4
    • 0001394987 scopus 로고
    • Wind-driven currents in a baroclinic ocean, with application to the equatorial currents of the eastern Pacific
    • Sverdrup, H. U., 1947: Wind-driven currents in a baroclinic ocean, with application to the equatorial currents of the eastern Pacific. Proc. Natl. Acad. Sci. U.S.A., 33, 318-326.
    • (1947) Proc. Natl. Acad. Sci. U.S.A. , vol.33 , pp. 318-326
    • Sverdrup, H.U.1
  • 5
    • 0001683682 scopus 로고
    • Model of world ocean circulation: Wind-driven, two-layer
    • Veronis, G., 1973: Model of world ocean circulation: wind-driven, two-layer. J. Mar. Res., 31, 228-288.
    • (1973) J. Mar. Res. , vol.31 , pp. 228-288
    • Veronis, G.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.