@InProceedings{SilvaBorMatAugRod:2015:EsCaBa,
author = "Silva, Ricardo Dal Agnol da and Borma, Laura de Simone and Mateus,
Pedro Jorge Bel{\'e} and Augusto-Silva, P{\'e}tala Bianchi and
Rodriguez, Daniel Andr{\'e}s",
affiliation = "{} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and {}
and {} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
title = "Estimativa da umidade do solo usando o modelo hidrol{\'o}gico
distribu{\'{\i}}do MHD-INPE: estudo de caso na Bacia do Purus",
booktitle = "Anais...",
year = "2015",
editor = "Gherardi, Douglas Francisco Marcolino and Arag{\~a}o, Luiz
Eduardo Oliveira e Cruz de",
pages = "4292--4299",
organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 17. (SBSR)",
publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
address = "S{\~a}o Jos{\'e} dos Campos",
abstract = "It is known that estimations of soil moisture with remote sensing
data (e.g. NDVI, land surface temperature) are restricted over
dense forested areas due to its interference with the remote
sensed signal. The use of process models like
soil-vegetation-atmosphere transfer or hydrological models may
contribute to minimize this problem and can be used to produce
more accurate soil moisture estimates. Therefore, the objective of
this study was to conduct preliminary analysis of the consistency
of soil moisture estimative by the distributed hydrologic model
MHD-INPE through the comparison with precipitation data. The model
succeeded in the representation of hydrological response of the
Purus Basin for 1970-1990 period, capturing the minimum and
maximum stream flow. The estimation of soil moisture using the
model showed a consistent spatial distribution in relation to the
precipitation. During the wet season, 60-day cumulative rainfall
presented a strong correlation with soil moisture, representing
the restitution of ground water stored in the soil. For the dry
season it was observed weaker correlations, as expected, due to
the absence of rainfall not mean low values of soil moisture. The
observed soil moisture in the dry season is related to ground
water already stored in the soil, which is decreased from the wet
season to the dry season due to factors such as lack of rainfall,
discharge from the aquifer and evapotranspiration processes.",
conference-location = "Jo{\~a}o Pessoa",
conference-year = "25-29 abr. 2015",
isbn = "978-85-17-0076-8",
label = "842",
language = "pt",
organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
ibi = "8JMKD3MGP6W34M/3JM4CKH",
url = "http://urlib.net/ibi/8JMKD3MGP6W34M/3JM4CKH",
targetfile = "p0842.pdf",
type = "Hidrologia",
urlaccessdate = "27 abr. 2024"
}