Computation of the Large Scale Vertical Velocity

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Authors
Haltiner, G.J.
Clarke, L.C.
Lawniczak, G.E.
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1963-04
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Abstract
Vertical velocities are computed at four levels over a Northern Hemisphere in addition to lower boundary value which is applied at terrain pressure and includes effects of frictionally- and terrain-induced vertical velocities. The latter, as computed here, have somewhat smaller maximum magnitudes and less irregularity than the frictionally-induced vertical velocity.
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The article of record as published may be found at http://dx.doi.org/10.1175/1520-0450(1963)002<0242:COTLSV>2.0.CO;2
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This research was supported in part by the Office of Naval Research.
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Journal of Applied Meteorology, Volume 2, pp. 242-259, April 1963.
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