On development in the field of barometri
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R. C. Sutcliffe
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Article
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2007
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John Wiley and Sons
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English
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## Abstract The rate of change of surface pressure is defined by the horizontal divergence of momentum integrated vertically through the entire atmosphere. As geostrophic winds are rigorously nonβdivergent, surface pressure cannot change when the motion is everywhere geostrophic (Jeffreys, 1919). P