Construct · 1 fields · 1 citations
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Geostrophic balance is the near-equilibrium, in large-scale flow away from the surface, between the horizontal pressure-gradient force and the Coriolis force, with the result that the wind blows nearly parallel to the isobars rather than straight from high to low pressure. Holton and Hakim's An introduction to dynamic meteorology presents this balance as the leading-order approximation for midlatitude synoptic winds, defining the geostrophic wind set by the pressure gradient and the Coriolis parameter. The referent is an idealised balanced wind used to read flow off a pressure map, exact only in the limit of slow, large-scale, frictionless motion.[1]
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