Evaluation of the Error of Sea Surface Temperature Estimate Algorithms, Using MODIS Data During Upwelling Events in Cabo Frio Coast, RJ

This work studies the uncertainties associated to sea surface temperature (SST) retrievals based on MODIS data, during the upwelling that normally occur alongside of coast of Cabo Frio, Brazil. The SST results versus the physical variables collected (or calculated from them) by Cabo Frio buoy (i...

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Main Authors: Gilberto Rodrigues Pimentel Junior, Gutemberg Borges França, Leonardo de Faria Peres
Format: Article
Language:English
Published: Universidade Federal do Rio de Janeiro 2018-12-01
Series:Anuário do Instituto de Geociências
Subjects:
Online Access:http://www.anuario.igeo.ufrj.br/2018_2/2018_2_31_40.pdf
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spelling doaj-f6c15684cbfb43aaa6c5524999144f6a2020-11-25T03:19:25ZengUniversidade Federal do Rio de JaneiroAnuário do Instituto de Geociências0101-97591982-39082018-12-014123140http://dx.doi.org/10.11137/2018_2_31_40Evaluation of the Error of Sea Surface Temperature Estimate Algorithms, Using MODIS Data During Upwelling Events in Cabo Frio Coast, RJGilberto Rodrigues Pimentel Junior0Gutemberg Borges França1Leonardo de Faria Peres2Universidade Federal do Rio de JaneiroUniversidade Federal do Rio de JaneiroUniversidade Federal do Rio de JaneiroThis work studies the uncertainties associated to sea surface temperature (SST) retrievals based on MODIS data, during the upwelling that normally occur alongside of coast of Cabo Frio, Brazil. The SST results versus the physical variables collected (or calculated from them) by Cabo Frio buoy (installed at 23º 37,82’ S; 42º 12,15’ W),from 1 January 2014 to 31 January 2015, were analysed. Results have indicated that upwelling occurrence – in the study area – is highly correlated with wind direction and also that the error in the estimation of sea surface temperature using satellite data is dependent on the difference between the air temperature and the in situ sea surface temperature (collected by buoy at 30 cm). An attempt to correct the mentioned error estimations suggested and discussedhttp://www.anuario.igeo.ufrj.br/2018_2/2018_2_31_40.pdfSea surface temperatureUpwellingMODIS
collection DOAJ
language English
format Article
sources DOAJ
author Gilberto Rodrigues Pimentel Junior
Gutemberg Borges França
Leonardo de Faria Peres
spellingShingle Gilberto Rodrigues Pimentel Junior
Gutemberg Borges França
Leonardo de Faria Peres
Evaluation of the Error of Sea Surface Temperature Estimate Algorithms, Using MODIS Data During Upwelling Events in Cabo Frio Coast, RJ
Anuário do Instituto de Geociências
Sea surface temperature
Upwelling
MODIS
author_facet Gilberto Rodrigues Pimentel Junior
Gutemberg Borges França
Leonardo de Faria Peres
author_sort Gilberto Rodrigues Pimentel Junior
title Evaluation of the Error of Sea Surface Temperature Estimate Algorithms, Using MODIS Data During Upwelling Events in Cabo Frio Coast, RJ
title_short Evaluation of the Error of Sea Surface Temperature Estimate Algorithms, Using MODIS Data During Upwelling Events in Cabo Frio Coast, RJ
title_full Evaluation of the Error of Sea Surface Temperature Estimate Algorithms, Using MODIS Data During Upwelling Events in Cabo Frio Coast, RJ
title_fullStr Evaluation of the Error of Sea Surface Temperature Estimate Algorithms, Using MODIS Data During Upwelling Events in Cabo Frio Coast, RJ
title_full_unstemmed Evaluation of the Error of Sea Surface Temperature Estimate Algorithms, Using MODIS Data During Upwelling Events in Cabo Frio Coast, RJ
title_sort evaluation of the error of sea surface temperature estimate algorithms, using modis data during upwelling events in cabo frio coast, rj
publisher Universidade Federal do Rio de Janeiro
series Anuário do Instituto de Geociências
issn 0101-9759
1982-3908
publishDate 2018-12-01
description This work studies the uncertainties associated to sea surface temperature (SST) retrievals based on MODIS data, during the upwelling that normally occur alongside of coast of Cabo Frio, Brazil. The SST results versus the physical variables collected (or calculated from them) by Cabo Frio buoy (installed at 23º 37,82’ S; 42º 12,15’ W),from 1 January 2014 to 31 January 2015, were analysed. Results have indicated that upwelling occurrence – in the study area – is highly correlated with wind direction and also that the error in the estimation of sea surface temperature using satellite data is dependent on the difference between the air temperature and the in situ sea surface temperature (collected by buoy at 30 cm). An attempt to correct the mentioned error estimations suggested and discussed
topic Sea surface temperature
Upwelling
MODIS
url http://www.anuario.igeo.ufrj.br/2018_2/2018_2_31_40.pdf
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