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Open AccessArticle

Decoupling between Precipitation Processes and Mountain Wave Induced Circulations Observed with a Vertically Pointing K-Band Doppler Radar

1
DT Catalonia, AEMET, 08005 Barcelona, Spain
2
Department of Applied Physics-Meteorology, University of Barcelona, 08028 Barcelona, Spain
3
Centre National de Recherches Météorologiques, METEO-FRANCE, CNRS, 31100 Toulouse, France
4
Snow and Mountain Research Center of Andorra, Institut d’Estudis Andorrans (CENMA-IEA), AD600 Sant Julià de Lòria, Andorra
*
Authors to whom correspondence should be addressed.
Remote Sens. 2019, 11(9), 1034; https://doi.org/10.3390/rs11091034
Received: 21 March 2019 / Revised: 24 April 2019 / Accepted: 26 April 2019 / Published: 1 May 2019
(This article belongs to the Special Issue Radar Meteorology)
Recent 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. View Full-Text
Keywords: MRR; Parsivel disdrometer; orographic precipitation; mountain waves; rotor; winter storm; Pyrenees MRR; Parsivel disdrometer; orographic precipitation; mountain waves; rotor; winter storm; Pyrenees
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MDPI and ACS Style

Gonzalez, S.; Bech, J.; Udina, M.; Codina, B.; Paci, A.; Trapero, L. Decoupling between Precipitation Processes and Mountain Wave Induced Circulations Observed with a Vertically Pointing K-Band Doppler Radar. Remote Sens. 2019, 11, 1034. https://doi.org/10.3390/rs11091034

AMA Style

Gonzalez S, Bech J, Udina M, Codina B, Paci A, Trapero L. Decoupling between Precipitation Processes and Mountain Wave Induced Circulations Observed with a Vertically Pointing K-Band Doppler Radar. Remote Sensing. 2019; 11(9):1034. https://doi.org/10.3390/rs11091034

Chicago/Turabian Style

Gonzalez, Sergi; Bech, Joan; Udina, Mireia; Codina, Bernat; Paci, Alexandre; Trapero, Laura. 2019. "Decoupling between Precipitation Processes and Mountain Wave Induced Circulations Observed with a Vertically Pointing K-Band Doppler Radar" Remote Sens. 11, no. 9: 1034. https://doi.org/10.3390/rs11091034

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