Evidence for vertical motions in the equatorial middle atmosphere.

M. L. Weisman, J. J. Olivero

Research output: Contribution to journalArticlepeer-review

3 Scopus citations

Abstract

The Diurnal Experiment, which took place in March 1974, offers a unique data set for use in studying vertical velocities in the equatoral stratsphere and mesosphere. Results suggest that modification of temperature and wind profiles in the stratosphere and lower mesosphere on an hourly basis can be quite significant. The analysis also suggests the presence of unresolved vertical winds on both longer and shorter time scales than the principal tidal components. -Authors

Original languageEnglish
Pages (from-to)2169-2182
Number of pages14
JournalJournal of the Atmospheric Sciences
Volume36
Issue number11
DOIs
StatePublished - 1979

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