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Volumn 29, Issue 3, 1999, Pages 512-518

Effect of a western continental slope on the wind-driven circulation

Author keywords

[No Author keywords available]

Indexed keywords

BOUNDARY CONDITIONS; CIRCULATION MODELING; CONTINENTAL SLOPE; TOPOGRAPHIC EFFECT; WIND-DRIVEN CIRCULATION;

EID: 0032721426     PISSN: 00223670     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0485(1999)029<0512:EOAWCS>2.0.CO;2     Document Type: Article
Times cited : (5)

References (12)
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    • Becker, J.M.1    Salmon, R.2
  • 2
    • 0027009870 scopus 로고
    • Inertial gyres in decaying and forced geostrophic turbulence
    • Cummins, P. F., 1992: Inertial gyres in decaying and forced geostrophic turbulence. J. Mar. Res., 50, 545-566.
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    • Cummins, P.F.1
  • 3
    • 0029414129 scopus 로고
    • Multiple solutions and advection-dominated flows in the wind-driven circulation. Part I: Slip
    • Ierley, G. R., and V. A. Sheremet, 1995: Multiple solutions and advection-dominated flows in the wind-driven circulation. Part I: Slip. J. Mar. Res., 53, 703-737.
    • (1995) J. Mar. Res. , vol.53 , pp. 703-737
    • Ierley, G.R.1    Sheremet, V.A.2
  • 4
    • 0030435948 scopus 로고    scopus 로고
    • Topographic ocean gyres: A western boundary slope
    • Kubokawa, A., and J. C. McWilliams, 1996: Topographic ocean gyres: A western boundary slope. J. Phys. Oceanogr., 26, 1468-1479.
    • (1996) J. Phys. Oceanogr. , vol.26 , pp. 1468-1479
    • Kubokawa, A.1    McWilliams, J.C.2
  • 5
    • 0021729559 scopus 로고
    • Third-order upwinding as a rational basis for computational fluid dynamics
    • J. Noye and C. Fletcher, Eds., Elsevier
    • Leonard, B. P., 1984: Third-order upwinding as a rational basis for computational fluid dynamics. Computational Techniques and Applications: CTAC-83, J. Noye and C. Fletcher, Eds., Elsevier, 106-120.
    • (1984) Computational Techniques and Applications: CTAC-83 , pp. 106-120
    • Leonard, B.P.1
  • 6
    • 0003044941 scopus 로고
    • On the wind-driven ocean circulation
    • Munk, W. H., 1950: On the wind-driven ocean circulation. J. Meteor., 7, 79-93.
    • (1950) J. Meteor. , vol.7 , pp. 79-93
    • Munk, W.H.1
  • 7
    • 84974178825 scopus 로고
    • How rapidly is a passive scalar mixed within closed streamlines?
    • Rhines, P. B., and W. R. Young, 1983: How rapidly is a passive scalar mixed within closed streamlines? J. Fluid Mech., 133, 133-145.
    • (1983) J. Fluid Mech. , vol.133 , pp. 133-145
    • Rhines, P.B.1    Young, W.R.2
  • 8
    • 0027009838 scopus 로고
    • A two-layer Gulf Stream over a continental slope
    • Salmon, R., 1992: A two-layer Gulf Stream over a continental slope. J. Mar. Res., 50, 341-365.
    • (1992) J. Mar. Res. , vol.50 , pp. 341-365
    • Salmon, R.1
  • 9
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    • Generalized two-layer models of ocean circulation
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  • 10
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    • Stommel, H.1
  • 11
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    • Wind-driven ocean circulation-part 2. Numerical solution of the nonlinear problem
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    • (1966) Deep-sea Res. , vol.13 , pp. 30-55
    • Veronis, G.1
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.