Mean winds in the tropical stratosphere and mesosphere during january 1993, march 1994, and august 1994

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dc.contributor.authorHitchman, M.
dc.contributor.authorKudeki, E.
dc.contributor.authorFritts, D. C.
dc.contributor.authorKugi, J. M.
dc.contributor.authorFawcett, C.
dc.contributor.authorPostel, G. A.
dc.contributor.authorYao, C.
dc.contributor.authorOrtland, D.
dc.contributor.authorRiggin, D.
dc.contributor.authorHarvey, V. L.
dc.date.accessioned2019-01-25T16:50:43Z
dc.date.available2019-01-25T16:50:43Z
dc.date.issued1997-11-27
dc.description.abstractRadar observations of winds and momentum fluxes in the stratosphere and mesosphere at the Jicamarca Radio Observatory in Peru ( JRO; 12S, 77W) were taken during three 10 day campaigns in January 1993, March 1994, and August 1994. In order to interpret features in the campaign mean JRO wind profiles, we examined global circulation patterns as depicted by long time series of radiosonde profiles, analyses from the European Center for Medium Range Weather Forecasting (ECMWF), and winds from the High Resolution Doppler Imager (HRDI) aboard the Upper Atmosphere Research Satellite. In the tropical stratosphere, large-scale analyses show that a geographically varying annual cycle significantly affects winds over JRO, as does the quasi-biennial oscillation ( QBO). The spatial structure of the annual cycle and QBO is shown for the three campaigns, emphasizing the upward influence of subtropical tropospheric monsoon anticyclones. These anticyclones tilt poleward and merge zonally, underlying the zonal summer easterlies, which also merge zonally and tilt poleward with altitude. The annual cycle at Singapore includes a substantial easterly acceleration during March-August, which causes an apparent stalling of descending QBO westerlies or a more rapid descent of QBO easterlies. In the mesosphere, JRO and HRDI winds agree reasonably well, with zonal winds over JRO varying on a semiannual basis and meridional winds exhibiting structures expected from the diurnal tide. For vertical motion, separate north-south and east-west beam pair estimates agree, yet campaign-averaged vertical motions are -1-5 cm/s in the stratosphere and -10-50 cm/s in the mesosphere. In both the stratosphere and mesosphere, vertical winds are anticorrelated with horizontal wind. Possible explanations for the large vertical motions include aspect sensitivity and the diurnal tide. Uncertainties in the meaning of radar vertical motions create a challenge for interpreting momentum fluxes.es_ES
dc.description.peer-reviewPor pareses_ES
dc.formatapplication/pdfes_ES
dc.identifier.citationHitchman, M., Kudeki, E., Fritts, D. C., Kugi, J. M., Fawcett, C., Postel, G. A., ... Harvey, V. L. (1997). Mean winds in the tropical stratosphere and mesosphere during january 1993, march 1994, and august 1994.==$Journal of Geophysical Research: Atmospheres, 102$==(D22), 26033-26052. https://doi.org/10.1029/97JD01784es_ES
dc.identifier.doihttps://doi.org/10.1029/97JD01784es_ES
dc.identifier.journalJournal of Geophysical Research: Atmosphereses_ES
dc.identifier.urihttp://hdl.handle.net/20.500.12816/3994
dc.language.isoenges_ES
dc.publisherAmerican Geophysical Uniones_ES
dc.relation.ispartofurn:issn:2169-897X
dc.rightsinfo:eu-repo/semantics/restrictedAccesses_ES
dc.subjectPolar Vortexes_ES
dc.subjectStratospherees_ES
dc.subjectZonal Windes_ES
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.01es_ES
dc.titleMean winds in the tropical stratosphere and mesosphere during january 1993, march 1994, and august 1994es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES

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