The relation between wind velocity at 1000 metres altitude and the surface pressure distribution
1908 ◽
Vol 80
(540)
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pp. 436-443
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Keyword(s):
For the steady horizontal motion of air along a path whose radius of curvature is r , we may write directly the equation (ω r sin λ ± v ) 2 / r = 1/ρ ∂ p / ∂ r +(ω r sin λ ) 2 / r , expressing the fact that the part of the centrifugal force arising from the motion of the wind is balanced by the effective gradient of pressure. In the equation p is atmospheric pressure, ρ density, v velocity of moving air, λ is latitude, and ω is the angular velocity of the earth about its axis.
2015 ◽
Vol 14
(0)
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pp. 43-51
2018 ◽
Vol 154
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pp. 1-9
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Keyword(s):
1963 ◽
Vol 67
(632)
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pp. 529-530
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Keyword(s):
2007 ◽
Vol 190
(1-3)
◽
pp. 263-281
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1996 ◽
Vol 62
(593)
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pp. 65-71
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2001 ◽
Vol 2001.13
(0)
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pp. 68-69
2003 ◽
Vol 2003.41
(0)
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pp. 107-108
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