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The barometric tides at Zürich and on the summit of Säntis

✍ Scribed by Bernhard Haurwitz; Ann D. Cowley

Publisher
Springer
Year
1975
Tongue
English
Weight
473 KB
Volume
113
Category
Article
ISSN
0033-4533

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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 non‐divergent, surface pressure cannot change when the motion is everywhere geostrophic (Jeffreys, 1919). P