Evaluation of effective eddy diffusive coefficients using radar observations of turbulence in the stratosphere

dc.contributor.authorWoodman Pollitt, Ronald Francisco
dc.contributor.authorRastogi, P.K.
dc.date.accessioned2018-06-25T12:23:16Z
dc.date.available2018-06-25T12:23:16Z
dc.date.issued1984-03
dc.description.abstractRadar observations show that thin persistent layers of turbulence occur sporadically in the troposphere and stratosphere. Two probabilistic approaches are used to show that the vertical eddy diffusivity due to such layers is of the order of 0.2-0.3 m²/sec in the lower stratosphere. An actual realization of turbulent layers, derived from the radar observations at Arecibo, is used in a numerical approach to obtain a profile of eddy diffusivity. It is suggested that turbulence plays a significant role in the vertical transport of trace constituents in the stratosphere.es_ES
dc.description.peer-reviewPor pareses_ES
dc.formatapplication/pdfes_ES
dc.identifier.citationWoodman, R. F., & Rastogi, P. K. (1984). Evaluation of effective eddy diffusive coefficients using radar observations of turbulence in the stratosphere.==$Geophysical Research Letter, 11$==(3), 243-246. https://doi.org/10.1029/GL011i003p00243es_ES
dc.identifier.doihttps://doi.org/10.1029/GL011i003p00243es_ES
dc.identifier.govdocindex-oti2018
dc.identifier.journalGeophysical Research Letterses_ES
dc.identifier.urihttp://hdl.handle.net/20.500.12816/1503
dc.language.isoenges_ES
dc.publisherAmerican Geophysical Uniones_ES
dc.relation.ispartofurn:issn:0094-8276
dc.rightsinfo:eu-repo/semantics/restrictedAccesses_ES
dc.subjectAtmospheric turbulencees_ES
dc.subjectTropospherees_ES
dc.subjectSpace radares_ES
dc.subjectTurbulent boundary layeres_ES
dc.subject.ocdehttp://purl.org/pe-repo/ocde/ford#1.05.01es_ES
dc.titleEvaluation of effective eddy diffusive coefficients using radar observations of turbulence in the stratospherees_ES
dc.typeinfo:eu-repo/semantics/articlees_ES

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