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- W2025182858 abstract "Abstract A scale analysis indicates that the cross-axial component of the vorticity equation reduces to a two-term expression: a buoyancy gradient term and a term involving the depth-derivative of the shear stress. We have computed surface stresses by integrating this equation between sill depth and the surface, assuming a negligible stress below sill depth. Whenever stratification is pronounced (N2≥3×10−4 sec−2), the surface stresses, thus computed using actual measurements, are in reasonably good agreement with the observed wind stresses at various seasons and locations." @default.
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- W2025182858 date "1974-10-01" @default.
- W2025182858 modified "2023-09-24" @default.
- W2025182858 title "Stress Distribution in the Red Sea and in the Gulf of Aqaba" @default.
- W2025182858 doi "https://doi.org/10.1175/1520-0485(1974)004<0663:sditrs>2.0.co;2" @default.
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