Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.11765/10560
Decoupling between precipitation processes and mountain wave induced circulations observed with a vertically pointing K-band Doppler radar
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dc.contributor.authorGonzález Herrero, Sergies_ES
dc.contributor.authorBech, Joanes_ES
dc.contributor.authorUdina, Mireiaes_ES
dc.contributor.authorCodina, B.es_ES
dc.contributor.authorPaci, Alexandrees_ES
dc.contributor.authorTrapero, L.es_ES
dc.date.accessioned2019-05-10T06:13:55Z-
dc.date.available2019-05-10T06:13:55Z-
dc.date.issued2019-
dc.identifier.citationRemote Sensing. 2019, 11(9), 1034es_ES
dc.identifier.issn2072-4292-
dc.identifier.urihttp://hdl.handle.net/20.500.11765/10560-
dc.description.abstractRecent studies reported that precipitation and mountain waves induced low tropospheric level circulations may be decoupled or masked by greater spatial scale variability despite generally there is a connection between microphysical processes of precipitation and mountain driven air flows. In this paper we analyse two periods of a winter storm in the Eastern Pyrenees mountain range (NE Spain) with different mountain wave induced circulations and low-level turbulence as revealed by Micro Rain Radar (MRR), microwave radiometer and Parsivel disdrometer data during the Cerdanya-2017 field campaign. We find that during the event studied mountain wave wind circulations and low-level turbulence do not affect neither the snow crystal riming or aggregation along the vertical column nor the surface particle size distribution of the snow. This study illustrates that precipitation profiles and mountain induced circulations may be decoupled which can be very relevant for either ground-based or spaceborne remote sensing of precipitation.es_ES
dc.description.sponsorshipThe Cerdanya-2017 field campaign is a research effort organized by the University of the Balearic Islands, the University of Barcelona, METEO-FRANCE and the Meteorological Service of Catalonia and was funded by the Spanish projects CGL2015-65627-C3-1-R (MINECO/FEDER), CGL2015-65627-C3-2-R (MINECO/FEDER), CGL2016-81828-REDT (MINECO) and the Water Research Institute (IdRA) of the University of Barcelona.es_ES
dc.language.isoenges_ES
dc.publisherMDPIes_ES
dc.rightsLicencia CC: Reconocimiento CC BYes_ES
dc.subjectMRRes_ES
dc.subjectParsivel disdrometeres_ES
dc.subjectOrographic precipitationes_ES
dc.subjectMountain waveses_ES
dc.subjectRotores_ES
dc.subjectWinter stormes_ES
dc.subjectPyreneeses_ES
dc.titleDecoupling between precipitation processes and mountain wave induced circulations observed with a vertically pointing K-band Doppler radares_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publisherversionhttps://dx.doi.org/10.3390/rs11091034es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
Appears in Collections:Artículos científicos 2019


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