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Assaf, Gad (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
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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    • 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.
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    • 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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