@Article{SchneebeliSBACMBM:2012:FiReCH,
author = "Schneebeli, M. and Sakuragi, Jojhy and Biscaro, Thiago Souza and
Angelis, C. F. and Carvalho da Costa, I. and Morales, C. and
Baldini, L. and Machado, Luiz Augusto Toledo",
affiliation = "Ecole Polytechnique F´ed´ erale de Lausanne (EPFL), School of
Architecture, Civil and Environmental Engineering (ENAC),
Lausanne, Switzerland and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {} and {} and Instituto de Astronomia, Geofisica e
Ci{\^e}ncias Atmosf{\'e}ricas, Universidade de S{\~a}o Paulo,
S{\~a}o Paulo, Brazil and nstituto di Scienze dell’Atmosfera e
del Clima (CNR), Rome, Italy and {Instituto Nacional de Pesquisas
Espaciais (INPE)}",
title = "Observations of tropical rain with a polarimetric X-band radar:
first results from the CHUVA campaign",
journal = "Atmospheric Measurement Techniques Discussions",
year = "2012",
volume = "5",
number = "1",
pages = "1717--1761",
note = "{Setores de Atividade: Pesquisa e desenvolvimento
cient{\'{\i}}fico.}",
keywords = "Polarimetric radar, Atenuation, Tropical rain.",
abstract = "A polarimetric X-band radar has been deployed during one month
(April 2011) for a field campaign in Fortaleza, Brazil, together
with additional sensors like a Ka-band vertically pointing
frequency modulated continuous wave (FMCW) radar and three laser
disdrometers. The disdrometers as well as the FMCW radar are
capable of measuring 5 the rain drop size distributions (DSDs),
hence making it possible to forward-model theoretical polarimetric
X-band radar observables at the point where the instruments are
located. This set-up allows to thoroughly test the accuracy of the
X-band radar measurements as well as the algorithms that are used
to correct the radar data for radome and rain attenuation. In the
first campaign in Fortaleza it was found that radome atten- 10
uation dominantly affects the measurements. With an algorithm that
is based on the self-consistency of the polarimetric observables,
the radome induced reflectivity offset was estimated. Offset
corrected measurements were then further corrected for rain
attenuation with two different schemes. The performance of the
post-processing steps is being analyzed by comparing the data with
disdrometer-inferred polarimetric variables 15 that were measured
in a distance of 20 km to the radar.",
doi = "10.5194/amtd-5-1717-2012",
url = "http://dx.doi.org/10.5194/amtd-5-1717-2012",
issn = "1867-8610",
label = "lattes: 5379515759830546 8 SchneebeliSBACMBM:2012:FiReCH",
language = "en",
targetfile = "amtd-5-1717-2012.pdf",
urlaccessdate = "30 abr. 2024"
}