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Assaf, Gad (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
The inertial theory of the Gulf Stream (Charney, 1955) is extended to include vertical friction in the cyclonic shear zone (the western side) of the stream. The vertical friction is assumed to be controlled by local Froude conditions.DOI: 10.1111/j.2153-3490.1977.tb00717.x
  • The results below are discovered through our pilot algorithms. Let us know how we are doing!

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    • Charney, J. G. 1955. The Gulf Stream as an inertial boundary layer. Proceedings of the National Academy of Sciences 41.73 1-740.
    • Defant, A. 1941. Die absolue Topographie des physikalshen Meeresniveaus und der Druckflachen, sowiedie Wasserbewegungen im Atlantischen Ozen, Deutsche Atlantishe Exped. Meteor, 1925-1927, Wiss., Eng., Bd 6 , 2 Tail, 5 Lief., Fig. 41.
    • Diiing, W. 1975. Synoptic studies of transients in the Florida current.J.Mar. Res. 33,53-73.
    • Fofonoff, N. B, 1954. Steady flow in a frictionless homogenous ocean.J.Mar. Res. 13,254262.
    • Hallock, 2. R. 1973. The kinetic energy balance of the Florida Straitsin a vertical section between Miami and Bimini, M.Sc. thesis, University of Miami Rosenstiel School of Marine and Atmospheric Sciences.
    • Lofquist, K. 1960. Flow and stress near interface between stratified liquids. Phys. ofFIuids 3, 158-175.
    • Munk, W. H. & Carrier, G. F. 1950. The winddriven circulation in ocean basins of various shapes. Tellus 2, 158-167.
    • Pillsbury, J. E. 1891. The Gulf Stream Rept. U.S. Cst. Gd. survey for 1890. AppendixNo. 10,461420.
    • Stem,M. E. 1972. Hydraulically critical rotating flow. Phys. of Fluids 15. 2062-2064.
    • Stommel, H . 1966. The Gurf Stream: A physical and dynamical description. University of California Press.
    • Thompson, R. 1973. Stratified Ekman Boundary layer models. Ceophys.Fluid Dyn. 201-210.
    • Turner, J. S. 1973. Buoyancy effects injluidr. Cambridge University Press.
    • Webster, F. 1965. Measurements of eddy fluxes Of momentum in the surface layer of the Gulf Stream. Tellus 17,23%245.
    • MHepwoHHaa Teopwrr ronb@TpwMa (YapHw, 1955) 0606~uae~cWflTeM BKJIlOYCHHII BepTHKWIbHOrO TpeHHII B 3 o ~ yUwKnoHwrecKoro c,qsnra CKopocTw (Ha 3anan~oZicTopose) crpyw. IIpemonaraeTca, YTO EpTHKWIbHOe TFHIle KOHTpOJIHpyeTCfl JIOKaJIbHbIM WCJIOM Qpyna.
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