@Article{OliveiraMaggVilaMora:2016:ChDiCy,
author = "Oliveira, R{\^o}mulo Augusto Juc{\'a} and Maggioni, Viviana and
Vila, Daniel Alejandro and Morales, Carlos",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {George
Mason University (GMU)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Universidade de S{\~a}o Paulo (USP)}",
title = "Characteristics and diurnal cycle of GPM rainfall estimates over
the central Amazon region",
journal = "Remote Sensing",
year = "2016",
volume = "8",
number = "7",
month = "July",
keywords = "satellite rainfall estimates, radar rainfall estimates, GPM,
IMERG, GPROF, uncertainty quantification, GoAmazon.",
abstract = "Studies that investigate and evaluate the quality, limitations and
uncertainties of satellite rainfall estimates are fundamental to
assure the correct and successful use of these products in
applications, such as climate studies, hydrological modeling and
natural hazard monitoring. Over regions of the globe that lack in
situ observations, such studies are only possible through
intensive field measurement campaigns, which provide a range of
high quality ground measurements, e.g., CHUVA (Cloud processes of
tHe main precipitation systems in Brazil: A contribUtion to cloud
resolVing modeling and to the GlobAl Precipitation Measurement)
and GoAmazon (Observations and Modeling of the Green Ocean Amazon)
over the Brazilian Amazon during 2014/2015. This study aims to
assess the characteristics of Global Precipitation Measurement
(GPM) satellite-based precipitation estimates in representing the
diurnal cycle over the Brazilian Amazon. The Integrated
Multi-satellitE Retrievals for Global Precipitation Measurement
(IMERG) and the Goddard Profiling Algorithm-Version 2014
(GPROF2014) algorithms are evaluated against ground-based radar
observations. Specifically, the S-band weather radar from the
Amazon Protection National System (SIPAM), is first validated
against the X-band CHUVA radar and then used as a reference to
evaluate GPM precipitation. Results showed satisfactory agreement
between S-band SIPAM radar and both IMERG and GPROF2014
algorithms. However, during the wet season, IMERG, which uses the
GPROF2014 rainfall retrieval from the GPM Microwave Imager (GMI)
sensor, significantly overestimates the frequency of heavy
rainfall volumes around 00:00-04:00 UTC and 15:00-18:00 UTC. This
overestimation is particularly evident over the Negro, Solimoes
and Amazon rivers due to the poorly-calibrated algorithm over
water surfaces. On the other hand, during the dry season, the
IMERG product underestimates mean precipitation in comparison to
the S-band SIPAM radar, mainly due to the fact that isolated
convective rain cells in the afternoon are not detected by the
satellite precipitation algorithm.",
doi = "10.3390/rs8070544",
url = "http://dx.doi.org/10.3390/rs8070544",
issn = "2072-4292",
language = "en",
targetfile = "Oliveira_characteristics.pdf",
urlaccessdate = "28 abr. 2024"
}