Gravity-wave generation by thunderstorms observed with a vertically-pointing 430 MHz radar

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dc.contributor.authorLarsen, M. F.
dc.contributor.authorSwartz, W.E.
dc.contributor.authorWoodman Pollitt, Ronald Francisco
dc.date.accessioned2016-10-17T21:30:32Z
dc.date.accessioned2017-12-21T19:41:39Z
dc.date.available2016-10-17T21:30:32Z
dc.date.available2017-12-21T19:41:39Z
dc.date.issued1982-05
dc.description.abstractDuring September of 1979, the Arecibo Observatory 430 MHz Doppler radar was used to study the upper troposphere and lower stratosphere during thunderstorm activity in the afternoon hours. It was found that when the olouds developed sufficiently in the vertical direction to reach the height of the tropopause, gravity-wave oscillations in the vertical velocity above the tropopause would develop. The amplitude was 2 m/s, and the period was close to 6 min.
dc.formatapplication/pdf
dc.identifier.citationLarsen, M. F., Swartz, W. E., & Woodman, R. F. (1982). Gravity-wave generation by thunderstorms observed with a vertically-pointing 430 MHz radar.==$Geophysical Research Letters, 9$==(5), 571-574. https://doi.org/10.1029/GL009i005p00571
dc.identifier.doihttps://doi.org/10.1029/GL009i005p00571
dc.identifier.journalGeophysical Research Letters
dc.identifier.urihttp://hdl.handle.net/20.500.12816/508
dc.language.isoeng
dc.publisherAmerican Geophysical Union
dc.relation.ispartofurn:issn:0094-8276
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectGravitational waves
dc.subjectStorms
dc.subjectRadar
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.01
dc.titleGravity-wave generation by thunderstorms observed with a vertically-pointing 430 MHz radar
dc.typeinfo:eu-repo/semantics/article

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