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- W2021763313 abstract "It is shown that if the flow on an isobaric surface is such that the wind and mass fields satisfy the gradient wind equation, then the gradient of the Bernoulli function (the sum of the kinetic energy per unit mass and the geopotential) is everywhere perpendicular to the local wind vector and that, furthermore, if the absolute vorticity is non-negative, the direction of increase of the Bernoulli function bears the same relation to the wind vector as does the direction of increase of the geopotential to the geostrophic wind. Applications of this relationship are discussed." @default.
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- W2021763313 date "1986-10-01" @default.
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- W2021763313 title "On the consequences of non-negative absolute vorticity" @default.
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- W2021763313 doi "https://doi.org/10.1002/qj.49711247418" @default.
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