CURIE: a low power X-band, low atmospheric Boundary Layer Doppler radar

A new X-band Doppler miniradar, the CURIE radar (Canopy Urban Research on Interactions and Exchanges), mainly adapted to low Atmospheric Boundary Layer ABL sounding has been developed at LATMOS (Laboratoire Atmosphères, Milieux, Observations Spatiales) formerly CETP (Centre d'étude des Environn...

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Main Authors: Hassan Al-Sakka, Alain Weill, Christophe Le Gac, Richard Ney, Laurent Chardenal, Jean Vinson, Laurent Paul Barthès, Eric Dupont
Format: Article
Language:English
Published: Borntraeger 2009-06-01
Series:Meteorologische Zeitschrift
Online Access:http://dx.doi.org/10.1127/0941-2948/2009/0377
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spelling doaj-dc804936f29e45ed9ee4ce98237d12782020-11-24T22:37:54ZengBorntraegerMeteorologische Zeitschrift0941-29482009-06-0118326727610.1127/0941-2948/2009/037773387CURIE: a low power X-band, low atmospheric Boundary Layer Doppler radarHassan Al-SakkaAlain WeillChristophe Le GacRichard NeyLaurent ChardenalJean VinsonLaurent Paul BarthèsEric DupontA new X-band Doppler miniradar, the CURIE radar (Canopy Urban Research on Interactions and Exchanges), mainly adapted to low Atmospheric Boundary Layer ABL sounding has been developed at LATMOS (Laboratoire Atmosphères, Milieux, Observations Spatiales) formerly CETP (Centre d'étude des Environnements Terrestre et Planétaires). After a brief description of the measurement conditions in a turbulent atmosphere, the main characteristics of the new sensor are presented. As an example, we compare CURIE vertical velocity fluctuations with UHF observations to show the vertical velocity measurement validity. As a prospective area of application in clear air, we focus on a first observation of vertical velocity variance which is supposed to be related to entrainment across the inversion layer. As our objective is to study low boundary layers during different atmospheric conditions and since the radar works in the presence of precipitation (as all X-band radar do), we also show vertical rain soundings in the lower part of the ABL and illustrate our findings with results demonstrating comparable reflectivity and precipitation rates as estimated with a disdrometer and with a rain gauge.http://dx.doi.org/10.1127/0941-2948/2009/0377
collection DOAJ
language English
format Article
sources DOAJ
author Hassan Al-Sakka
Alain Weill
Christophe Le Gac
Richard Ney
Laurent Chardenal
Jean Vinson
Laurent Paul Barthès
Eric Dupont
spellingShingle Hassan Al-Sakka
Alain Weill
Christophe Le Gac
Richard Ney
Laurent Chardenal
Jean Vinson
Laurent Paul Barthès
Eric Dupont
CURIE: a low power X-band, low atmospheric Boundary Layer Doppler radar
Meteorologische Zeitschrift
author_facet Hassan Al-Sakka
Alain Weill
Christophe Le Gac
Richard Ney
Laurent Chardenal
Jean Vinson
Laurent Paul Barthès
Eric Dupont
author_sort Hassan Al-Sakka
title CURIE: a low power X-band, low atmospheric Boundary Layer Doppler radar
title_short CURIE: a low power X-band, low atmospheric Boundary Layer Doppler radar
title_full CURIE: a low power X-band, low atmospheric Boundary Layer Doppler radar
title_fullStr CURIE: a low power X-band, low atmospheric Boundary Layer Doppler radar
title_full_unstemmed CURIE: a low power X-band, low atmospheric Boundary Layer Doppler radar
title_sort curie: a low power x-band, low atmospheric boundary layer doppler radar
publisher Borntraeger
series Meteorologische Zeitschrift
issn 0941-2948
publishDate 2009-06-01
description A new X-band Doppler miniradar, the CURIE radar (Canopy Urban Research on Interactions and Exchanges), mainly adapted to low Atmospheric Boundary Layer ABL sounding has been developed at LATMOS (Laboratoire Atmosphères, Milieux, Observations Spatiales) formerly CETP (Centre d'étude des Environnements Terrestre et Planétaires). After a brief description of the measurement conditions in a turbulent atmosphere, the main characteristics of the new sensor are presented. As an example, we compare CURIE vertical velocity fluctuations with UHF observations to show the vertical velocity measurement validity. As a prospective area of application in clear air, we focus on a first observation of vertical velocity variance which is supposed to be related to entrainment across the inversion layer. As our objective is to study low boundary layers during different atmospheric conditions and since the radar works in the presence of precipitation (as all X-band radar do), we also show vertical rain soundings in the lower part of the ABL and illustrate our findings with results demonstrating comparable reflectivity and precipitation rates as estimated with a disdrometer and with a rain gauge.
url http://dx.doi.org/10.1127/0941-2948/2009/0377
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