@Article{CalheirosMach:2014:ClRaLi,
author = "Calheiros, Alan J. P. and Machado, Luiz Augusto Toledo",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "Cloud and rain liquid water statistics in the CHUVA campaign",
journal = "Atmospheric Research",
year = "2014",
volume = "144",
pages = "126--140",
keywords = "cloud liquid water, cloud types, droplet size distribution, radar,
radiometer.",
abstract = "The purpose of this study is to present statistics related to the
integration of cloud and rain liquid water and the profiles for
different cloud types and regimes. From 2010 to 2012, the CHUVA
project collected information regarding cloud and rain
characteristics in different precipitation regimes in Brazil.
CHUVA had four field campaigns between 2010 and 2011, located in
the North, Northeast and Southeast regions of Brazil, covering the
semi-arid, Amazon, coastal and mountain regions. The synergy of
several instruments allowed us to classify rain events and
describe the cloud processes regionally. Microwave radiometers,
LiDAR, radar, and disdrometers were employed in this study. The
rain type classification was made using vertical profiles of
reflectivity (VPR) and polarimetric variables from dual
polarization radar (XPOL). The integrated liquid water (ILWC) for
non-precipitating clouds was retrieved with a microwave
ground-based radiometer using a neural network. For rainy
conditions, the profiles from the rain liquid water content (LWCR)
and their integrated (ILWR) properties were estimated by Micro
Rain Radar (MRR) and XPOL VPRs. For non-precipitating clouds, the
ILWC values were larger for the sites in tropical regions, in
particular near the coast, than for Southeast Brazil. For rainy
cases, distinct LWCR profiles were observed for different rain
classifications and regions. The differences are small for low
rain rates and a distinction between different rainfall regimes is
more evident for high rain rates. Vale and Bel{\'e}m clouds
present the deepest layers and largest convective rain rates. The
clouds in the Southeast region of Brazil (Vale do
Para{\'{\i}}ba) and North region (Bel{\'e}m) showed the largest
reflectivity in the mixed and glaciated layers, respectively. In
contrast, the Northeast coastal site (e.g. Fortaleza) showed
larger values in the warm part of the clouds. Several analyses are
presented, describing the cloud processes and the differences
among the cloud types, rain rates and regions.",
doi = "10.1016/j.atmosres.2014.03.006",
url = "http://dx.doi.org/10.1016/j.atmosres.2014.03.006",
issn = "0169-8095",
label = "scopus 2014-05 CalheirosMach:2014:ClRaLi",
language = "en",
url = "http://dx.doi.org/10.1016/j.atmosres.2014.03.006",
urlaccessdate = "27 abr. 2024"
}