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dc.contributor.authorWooldridge, Gene L.
dc.contributor.authorReiter, Elmar R.
dc.contributor.institutionColorado State University. Department of Atmospheric Science
dc.contributor.institutionColorado State University. Department of Civil Engineering
dc.date.accessioned2019-10-11T18:09:41Z
dc.date.available2019-10-11T18:09:41Z
dc.date.issued1970-09
dc.descriptionCER70-71GLW28.
dc.descriptionSeptember, 1970.
dc.descriptionThis report was prepared with support under contract number NAS 9-10305 National Aeronautics and Space Administration.
dc.description.abstractHigh-resolution pictures obtained with a handheld camera during the earth-orbital photographic mission of the Apollo IX spacecraft provided a unique opportunity to map the areal extent of gravity waves over the southwestern United States. The orientation of cumulus streets and cirrus streaks augmented conventional wind data for momentum and kinetic energy calculations. Zonal shearing stress gradients in stably stratified air flowing over rugged mountainous terrain indicated very large subgrid-scale vertical fluxes of zonal momentum. Maximum stress values of several tens of dynes cm-2 occurred in the lower tropospheric layers where the air flow encountered the high Rocky Mountains of central New Mexico. The vertical fluxes of zonal momentum were directed upward to tropopause levels when extensive areas of gravity waves covered eastern Arizona, New Mexico, and western Texas. The potential energy contained in the wave population 5-2 attained values through the troposphere as high as 9.3 x 10 joules m 8-2 (9.3 x 10 ergs cm); this potential energy apparently played a substantial role in the energy budget. The residual "dissipation" term in the kinetic energy budget indicated a subgrid-scale flux of energy downward from the lower stratosphere concurrent with the upward flux of zonal momentum. Atmospheric turbulence rose to a maximum intensity during the wave occurrence, diminishing gradually thereafter.
dc.description.sponsorshipUnder contract number NAS 9-10305.
dc.format.mediumtechnical reports
dc.identifier.urihttps://hdl.handle.net/10217/198259
dc.languageEnglish
dc.publisherColorado State University. Libraries
dc.publisher.originalDept. of Atmospheric Science, Colorado State University
dc.relationCatalog record number (MMS ID): 991023632699703361
dc.relation.ispartofCivil Engineering Reports
dc.relation.ispartofCER; 70/71-28
dc.subject.lcshGravity waves
dc.subject.lcshAtmospheric circulation -- Effect of mountains on
dc.titleVertical momentum transport over mountainous terrain
dc.typeText


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