Characterization of the precipitation in southwestern part of Greece with X-band Doppler radar, 2-D video disdrometer and rain gauges

We document precipitation in the southwestern part of Greece with the National Observatory of Athens (NOA) X-band radar, NOA 2D video disdrometer and a network of rain gauges. The observations were collected between February and April 2004. Time evolution of the drop size distribution (DSD) is prese...

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Main Authors: E. Defer, M. Anagnostou
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/7/121/2006/adgeo-7-121-2006.pdf
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author E. Defer
M. Anagnostou
author_facet E. Defer
M. Anagnostou
author_sort E. Defer
collection DOAJ
description We document precipitation in the southwestern part of Greece with the National Observatory of Athens (NOA) X-band radar, NOA 2D video disdrometer and a network of rain gauges. The observations were collected between February and April 2004. Time evolution of the drop size distribution (DSD) is presented for the 9 March 2004 case where rain rate (computed on 1-min period) was measured up to 80 mm/h and reflectivity at the location of the disdrometer exceeded 40 dBZ. We then present the differences of DSD as function of the rain rate for the studied case as well as for the entire observations of the field experiment. It shows that higher the rain rate is, larger the range of the DSD and higher the concentration of the raindrops are.
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spelling doaj.art-e4f76b197a2a41028f62ddfc432a6a872022-12-22T02:45:42ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592006-01-017121125Characterization of the precipitation in southwestern part of Greece with X-band Doppler radar, 2-D video disdrometer and rain gaugesE. DeferM. AnagnostouWe document precipitation in the southwestern part of Greece with the National Observatory of Athens (NOA) X-band radar, NOA 2D video disdrometer and a network of rain gauges. The observations were collected between February and April 2004. Time evolution of the drop size distribution (DSD) is presented for the 9 March 2004 case where rain rate (computed on 1-min period) was measured up to 80 mm/h and reflectivity at the location of the disdrometer exceeded 40 dBZ. We then present the differences of DSD as function of the rain rate for the studied case as well as for the entire observations of the field experiment. It shows that higher the rain rate is, larger the range of the DSD and higher the concentration of the raindrops are.http://www.adv-geosci.net/7/121/2006/adgeo-7-121-2006.pdf
spellingShingle E. Defer
M. Anagnostou
Characterization of the precipitation in southwestern part of Greece with X-band Doppler radar, 2-D video disdrometer and rain gauges
Advances in Geosciences
title Characterization of the precipitation in southwestern part of Greece with X-band Doppler radar, 2-D video disdrometer and rain gauges
title_full Characterization of the precipitation in southwestern part of Greece with X-band Doppler radar, 2-D video disdrometer and rain gauges
title_fullStr Characterization of the precipitation in southwestern part of Greece with X-band Doppler radar, 2-D video disdrometer and rain gauges
title_full_unstemmed Characterization of the precipitation in southwestern part of Greece with X-band Doppler radar, 2-D video disdrometer and rain gauges
title_short Characterization of the precipitation in southwestern part of Greece with X-band Doppler radar, 2-D video disdrometer and rain gauges
title_sort characterization of the precipitation in southwestern part of greece with x band doppler radar 2 d video disdrometer and rain gauges
url http://www.adv-geosci.net/7/121/2006/adgeo-7-121-2006.pdf
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