@Article{MiguelRenn:2020:UsDaRa,
author = "Miguel, B{\'a}rbara Hass and Renn{\'o}, Camilo Daleles",
affiliation = "{Universidade de Bras{\'{\i}}lia (UnB)} and {Instituto Nacional
de Pesquisas Espaciais (INPE)}",
title = "Uso de dados de radar meteorol{\'o}gico em modelo
hidrol{\'o}gico SCS-CN para a estimativa de escoamento
superficia",
journal = "Revista Brasileira de Cartografia",
year = "2020",
volume = "72",
number = "3",
pages = "501--516",
keywords = "Modelo hidrol{\'o}gicoSCS-CN. Radar meteorol{\'o}gico. Chuva
efetiva. Bacia hidrogr{\'a}fica, SCS-CN Hydrological Model.
Weather radar. Effective rainfall. Watershed.",
abstract = "Oobjetivo do presente trabalho foiavaliara viabilidade do uso de
estimativas de chuva a partir de dados do radar meteorol{\'o}gico
do Instituto de Pesquisas Meteorol{\'o}gicas de Bauru
(IPMet/UNESP) na implementa{\c{c}}{\~a}o do modelo
hidrol{\'o}gico distribu{\'{\i}}do simplificado Soil
Conservation ServiceCurve Number(SCS-CN),a fim de se analisar o
escoamento superficial de eventos de precipita{\c{c}}{\~a}o na
bacia hidrogr{\'a}fica do Rio Jacar{\'e}-Gua{\c{c}}u,
localizada na regi{\~a}o centro-leste do estado de S{\~a}o
Paulo.Nesse trabalho, as estimativas de chuva a partir de dados do
radar meteorol{\'o}gico do IPMetforamcalibradas comdados de 18
esta{\c{c}}{\~o}es pluviom{\'e}tricas, contudo, a {\'a}rea de
estudo apresenta apenas uma esta{\c{c}}{\~a}o fluviom{\'e}trica
em opera{\c{c}}{\~a}o, localizada no exut{\'o}rio da
bacia.Foram escolhidos doiseventos ocorridos em janeiro e
fevereiro de 2013, de acordo com a propaga{\c{c}}{\~a}o do
escoamento superficial extra{\'{\i}}do a partirda
aplica{\c{c}}{\~a}o de umfiltro digital de separa{\c{c}}{\~a}o
de escoamento. Osresultados foram satisfat{\'o}rios em
rela{\c{c}}{\~a}o a propaga{\c{c}}{\~a}o do escoamento
superficial gerada pelo modelo hidrol{\'o}gico SCS-CN.Entretanto,
{\'e}preciso ressaltar que alguns fatores de incerteza foram
levados em considera{\c{c}}{\~a}o no processo de
implementa{\c{c}}{\~a}o do modelo hidrol{\'o}gico. Um desses
fatores{\'e} que a falta decalibra{\c{c}}{\~a}o de
par{\^a}metros do modelo SCS-CN, como os valores tabelados da CN,
pode ter produzido alguns valores esp{\'u}rios de chuva efetiva
e, consequentemente, isso pode ter interferido nos valores de
propaga{\c{c}}{\~a}o do escoamento superficial. ABSTRACT: The
aim of the present work was to evaluate the feasibility of using
rain based on meteorological radar data from the Institute of
Meteorological Research of Bauru (IPMet / UNESP) in the
implementation of the simplified distributed hydrological model
Soil Conservation Service -Curve Number (SCS) -CN), an end of
analysis or runoff of events in the Jacar{\'e}-Gua{\c{c}}u River
watershed, located in the central-eastern region of the S{\~a}o
PauloState. In this work, how to display rain from IPMet weather
radar data was calibrated with data from 18 rainfall stations,
however, a study area has only one fluviometric station in
operation, located outside the basin. Two events that took place
in January and February 2013 were selected, according to the
spread runoff extracted from the application of a digital runoff
selection filter. The results were satisfactory aboutthe
propagation of runoff generated by the hydrological model SCS-CN.
However, it should be noted that some factors of uncertainty were
taken into account in the process of implementing the hydrological
model. One of these factors is the lack of calibration of the
parameters of the SCS-CN model, such as the tabulated values of
the CN, which may produce some spurious data of the effective rain
and, consequently, this may have interfered with the values of
propagation of the runoff.",
doi = "10.14393/rbcv72n3-53684",
url = "http://dx.doi.org/10.14393/rbcv72n3-53684",
issn = "0560-4613 and 1808-0936",
language = "pt",
targetfile = "miguel_uso.pdf",
urlaccessdate = "19 abr. 2024"
}