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dc.contributor.authorHaltiner, G.J.
dc.contributor.authorClarke, L.C.
dc.contributor.authorLawniczak, G.E.
dc.date.accessioned2015-08-04T22:18:28Z
dc.date.available2015-08-04T22:18:28Z
dc.date.issued1963-04
dc.identifier.citationJournal of Applied Meteorology, Volume 2, pp. 242-259, April 1963.
dc.identifier.urihttp://hdl.handle.net/10945/45756
dc.descriptionThe article of record as published may be found at http://dx.doi.org/10.1175/1520-0450(1963)002<0242:COTLSV>2.0.CO;2en_US
dc.description.abstractVertical 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.en_US
dc.description.sponsorshipThis research was supported in part by the Office of Naval Research.en_US
dc.titleComputation of the Large Scale Vertical Velocityen_US


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