High-altitude-resolution stratospheric measurements with the Arecibo 2380-MHz radar

dc.contributor.authorWoodman Pollitt, Ronald Francisco
dc.date.accessioned2016-10-25T22:36:34Z
dc.date.accessioned2017-12-21T19:41:45Z
dc.date.available2016-10-25T22:36:34Z
dc.date.available2017-12-21T19:41:45Z
dc.date.issued1980-03
dc.description.abstractThe 2380-MHz planetary radar of the Arecibo Observatory and the 30-m interferometer antenna at Higuialles, Puerto Rico, have been instrumented. as a .bistatic radar for stratosphenc turbulence research studies. The average power of the transmitter is 400 kW, and it uses the 300-m Arecibo spherical reflector. A vertical resolution of 30 m has been achieved by means of a novel continuous pseudorandom phase coding scheme. Preliminary results obtamed with the system are presented. The thickness and internal structure of turbulent stratosphcric layers have been resolved for the first time. The potential of the instrument in assessing the role of turbulence in the vertical transport of tracers, contaminants, and momentum is discussed.
dc.description.sponsorshipROJ
dc.formatapplication/pdf
dc.identifier.citationWoodman, R. F. (1980). High-altitude-resolution stratospheric measurements with the Arecibo 2380-MHz radar.==$Radio Science, 15$==(2), 423-430. https://doi.org/10.1029/RS015i002p00423
dc.identifier.doihttps://doi.org/10.1029/RS015i002p00423
dc.identifier.journalRadio Science
dc.identifier.urihttp://hdl.handle.net/20.500.12816/565
dc.language.isoeng
dc.publisherAmerican Geophysical Union
dc.relation.ispartofurn:issn:0048-6604
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectRadar
dc.subjectInterferometry
dc.subjectStratosphere
dc.subjectTurbulence
dc.subjectWinds
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.01
dc.titleHigh-altitude-resolution stratospheric measurements with the Arecibo 2380-MHz radar
dc.typeinfo:eu-repo/semantics/article

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