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Volumn 26, Issue 8, 1996, Pages 1579-1590

The vertical structure of turbulent dissipation in shelf seas

Author keywords

[No Author keywords available]

Indexed keywords

COLUMNS; TIDAL WATERS; TURBULENCE;

EID: 0030434870     PISSN: 00223670     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0485(1996)026<1579:TVSOTD>2.0.CO;2     Document Type: Article
Times cited : (187)

References (12)
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    • (1987) Contin. Shelf Res. , vol.7 , pp. 643-683
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  • 2
    • 0028174774 scopus 로고
    • On the practical advantages of the quasi-equilibrium version of the Mellor and Yamada level 2.5 closure applied to marine modelling
    • Deleersnijder, E., and P. Luyten, 1994: On the practical advantages of the quasi-equilibrium version of the Mellor and Yamada level 2.5 closure applied to marine modelling. Appl. Math. Modelling, 18, 281-287.
    • (1994) Appl. Math. Modelling , vol.18 , pp. 281-287
    • Deleersnijder, E.1    Luyten, P.2
  • 3
    • 0000782311 scopus 로고
    • Bottom stress estimates from vertical dissipation rate profiles on the Continental Shelf
    • Dewey, R. K., and W. R. Crawford, 1988: Bottom stress estimates from vertical dissipation rate profiles on the Continental Shelf. J. Phys. Oceanogr., 18, 1167-1177.
    • (1988) J. Phys. Oceanogr. , vol.18 , pp. 1167-1177
    • Dewey, R.K.1    Crawford, W.R.2
  • 4
    • 0023144271 scopus 로고
    • A microstructure instrument for profiling oceanic turbulence in coastal bottom boundary layers
    • _, _, A. E. Gargett, and N. S. Oakey, 1987: A microstructure instrument for profiling oceanic turbulence in coastal bottom boundary layers. J. Atmos. Oceanic Technol., 4, 288-297.
    • (1987) J. Atmos. Oceanic Technol. , vol.4 , pp. 288-297
    • Gargett, A.E.1    Oakey, N.S.2
  • 5
    • 0029657275 scopus 로고    scopus 로고
    • Presentation of a family of turbulence closure models of stratified shallow water flows and application to the Rhine outflow region
    • Lutyen, P. J., E. Deleersnijder, J. Ozer, and K. G. Ruddick, 1996: Presentation of a family of turbulence closure models of stratified shallow water flows and application to the Rhine outflow region. Contin. Shelf Res., 16, 101-130.
    • (1996) Contin. Shelf Res. , vol.16 , pp. 101-130
    • Lutyen, P.J.1    Deleersnijder, E.2    Ozer, J.3    Ruddick, K.G.4
  • 6
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    • Mellor, G. L., and T. Yamada, 1974: A hierarchy of turbulence closure models for planetary boundary layers. J. Atmos. Sci., 31, 1791-1806.
    • (1974) J. Atmos. Sci. , vol.31 , pp. 1791-1806
    • Mellor, G.L.1    Yamada, T.2
  • 7
    • 0004221696 scopus 로고
    • Ph.D. thesis, University of British Columbia
    • Nasmyth, P. W., 1970: Oceanic turbulence. Ph.D. thesis, University of British Columbia, 105 pp.
    • (1970) Oceanic Turbulence
    • Nasmyth, P.W.1
  • 8
    • 0006749391 scopus 로고
    • The depth averaged residual circulation on the North West European Shelf
    • Available from Bidston Observatory, Birkenhead, Merseyside L43 7RA, United Kingdom
    • Proctor, R., and J. A. Smith, 1991: The depth averaged residual circulation on the North West European Shelf. Proudman Oceanographic Laboratory Rep. 20, 255 pp. [Available from Bidston Observatory, Birkenhead, Merseyside L43 7RA, United Kingdom.]
    • (1991) Proudman Oceanographic Laboratory Rep. 20
    • Proctor, R.1    Smith, J.A.2
  • 9
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    • The role of tidal stirring in controlling the seasonal heat cycle in shelf seas
    • Simpson, J. H., and D. G. Bowers, 1984: The role of tidal stirring in controlling the seasonal heat cycle in shelf seas. Ann. Geophys., 2, 411-416.
    • (1984) Ann. Geophys. , vol.2 , pp. 411-416
    • Simpson, J.H.1    Bowers, D.G.2
  • 10
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    • Dynamically active models in the prediction of estuarine stratification
    • D. Prandle, Ed., Amer. Geophys. Union
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    • (1992) Dynamics and Exchanges in Estuaries and the Coastal Zone , pp. 101-113
    • Sharples, J.1
  • 11
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    • _, _, and T. P. Rippeth, 1991: A prescriptive model of stratification induced by freshwater run-off. Estuar. Coastal Shelf Sci., 33, 23-35.
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.