@InProceedings{SilvaManzAlbu:2019:MoEvIm,
author = "Silva, C{\'e}sar de Oliveira Ferreira and Manzione, Rodrigo Lilla
and Albuquerque Filho, Jos{\'e} Luiz",
affiliation = "{Universidade Estadual Paulista (UNESP)} and {Universidade
Estadual Paulista (UNESP)} and {Instituto de Pesquisas
Tecnol{\'o}gicas (IPT)}",
title = "Modelagem da evapotranspira{\c{c}}{\~a}o com imagens Santinel-2
e Landsat-8",
booktitle = "Anais...",
year = "2019",
editor = "Gherardi, Douglas Francisco Marcolino and Sanches, Ieda DelArco
and Arag{\~a}o, Luiz Eduardo Oliveira e Cruz de",
pages = "1584--1587",
organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 19. (SBSR)",
publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
address = "S{\~a}o Jos{\'e} dos Campos",
keywords = "uso da {\'a}gua, irriga{\c{c}}{\~a}o, R, Water use, irrigation,
R.",
abstract = "A modelagem de evapotranspira{\c{c}}{\~a}o (ET) foi realizada
por meio do algoritmo SAFER (Surface Algorithm for
Evapotranspiration Retrieving) com imagens de sat{\'e}lite
Landsat e Sentinel-2 do mesmo dia (26 de novembro de 2016), no
Sudeste do Brasil, avaliando se houve diferen{\c{c}}as
significativas entre essas fontes de dados radiom{\'e}tricos. O
albedo superficial variou de 0,12 a 0,29. O NDVI variou de -0,43 a
0,85. Evapotranspira{\c{c}}{\~a}o atingiu at{\'e} 4,7 mm e a
temperatura superficial variou entre 300 e 345 K. N{\~a}o houve
diferen{\c{c}}a significativa entre a utiliza{\c{c}}{\~a}o do
Sentinel-2 e Landsat-8 para modelagem do albedo superficial nem
entre o uso da banda termal e do m{\'e}todo residual com
reflect{\^a}ncias do Landsat-8, mas houve para o NDVI,
evapotranspira{\c{c}}{\~a}o e outros casos da temperatura
superficial. ABSTRACT: Evapotranspiration (ET) modeling was
performed by the socalled SAFER algorithm (Surface Algorithm for
Evapotranspiration Retrieving) with satellite images of Landsat-8
and Sentinel-2 of the same day (November 26, 2016) in Southeastern
Brazil, evaluating whether there were significant differences
between those sources of radiometric data. The surface albedo
ranged from 0,12 to 0,29. NDVI ranged from -0,43 to 0,85.
Evapotranspiration reached 4.7 mm and a surface temperature
varying between 300 and 345 K. Evapotranspiration reached up to
4.7 mm and the surface temperature varied between 300 and 345 K.
There was no significant difference between the use of Sentinel-2
and Landsat-8 for modeling the superficial albedo nor between the
use of the thermal band and the residual method with Landsat-8
reflectances, but there was for NDVI, evapotranspiration and other
cases of surface temperature.",
conference-location = "Santos",
conference-year = "14-17 abril 2019",
isbn = "978-85-17-00097-3",
language = "pt",
organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
ibi = "8JMKD3MGP6W34M/3U62QR8",
url = "http://urlib.net/ibi/8JMKD3MGP6W34M/3U62QR8",
targetfile = "97655.pdf",
type = "Monitoramento e modelagem ambiental",
urlaccessdate = "13 maio 2024"
}