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dc.contributor.author Larsen, M. F.
dc.contributor.author Swartz, W.E.
dc.contributor.author Woodman Pollitt, Ronald Francisco
dc.date.accessioned 2016-10-17T21:30:32Z
dc.date.accessioned 2017-12-21T19:41:39Z
dc.date.available 2016-10-17T21:30:32Z
dc.date.available 2017-12-21T19:41:39Z
dc.date.issued 1982-05
dc.identifier.citation Larsen, 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 es_ES
dc.identifier.uri http://hdl.handle.net/20.500.12816/508
dc.description.abstract During 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. es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher American Geophysical Union es_ES
dc.relation.ispartof urn:issn:0094-8276
dc.rights info:eu-repo/semantics/restrictedAccess es_ES
dc.subject Gravitational waves es_ES
dc.subject Storms es_ES
dc.subject Radar es_ES
dc.title Gravity-wave generation by thunderstorms observed with a vertically-pointing 430 MHz radar es_ES
dc.type info:eu-repo/semantics/article es_ES
dc.subject.ocde http://purl.org/pe-repo/ocde/ford#1.05.01 es_ES
dc.identifier.journal Geophysical Research Letters es_ES
dc.identifier.doi https://doi.org/10.1029/GL009i005p00571 es_ES

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