Study of the surface water circulation in San Blas channel (Argentina) using landsat imagery

This paper deals with the application of satellite images to study turbidity and water circulation patterns in San Blas channel during a theoretical tidal cycle. Eight Landsat TM and ETM images acquired under clear-sky conditions and representing different tidal stages were selected from a pool of L...

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Main Authors: Débora Beigt, Diana G. Cuadrado, María C. Piccolo
Format: Article
Language:English
Published: Universidade de São Paulo 2011-09-01
Series:Brazilian Journal of Oceanography
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1679-87592011000300004
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author Débora Beigt
Diana G. Cuadrado
María C. Piccolo
author_facet Débora Beigt
Diana G. Cuadrado
María C. Piccolo
author_sort Débora Beigt
collection DOAJ
description This paper deals with the application of satellite images to study turbidity and water circulation patterns in San Blas channel during a theoretical tidal cycle. Eight Landsat TM and ETM images acquired under clear-sky conditions and representing different tidal stages were selected from a pool of Landsat images provided by the argentinean National Commission of Space Activities (CONAE) and the US Geological Survey. Standard digital image processing techniques were used to perform geometric and radiometric corrections on the visible and near-infrared bands. An image-based atmospheric correction (COST method by CHAVEZ, 1996) was applied. An ISODATA unsupervised classification was performed in order to identify different turbidity levels throughout the channel and adjacent areas. The results suggest that suspended sediment transport towards the channel mouth by ebb currents occurs along both flanks. These currents carry suspended sediment into the open sea, generating an ebb tidal delta which tends to rotate in a clockwise direction. Flood currents trigger turbidity mostly over the southern flank of the channel, generating a flood tidal delta with elongated banks extending in the direction of the tidal currents. From the elongated shape of the turbidity plumes, general tidal circulation patterns were identified.<br>Este trabalho analisa a turbidez e a circulação da agua no canal San Blas durante um ciclo de maré teórico através de imagens satelitais. Foram utilizadas 8 imagens Landsat TM e ETM adquiridas em condições de céu claro e ao longo de diferentes momentos da maré. As imagens foram proporcionadas pela Comisión Nacional de Actividades Espaciales (CONAE) y pelo Serviço Geológico dos Estados Unidos (USGS). As correções geométricas e radiométricas foram realizadas nas bandas do espectro visível e do infravermelho próximo, utilizando técnicas padrões de processamento digital. Foi aplicada a correção atmosférica COST (CHAVEZ, 1996). Foi realizada uma classificação ISODATA não supervisionada para identificar diferentes níveis de turbidez al longo do canal e zonas adjacentes. Os resultados sugerem que o transporte de sedimento em suspensão para a boca do canal se da ao longo de ambos flancos, pela ação das correntes de refluxo. Estas correntes geram um delta de refluxo com uma tendência de rotação para a direção sul. As correntes de fluxo provocam turbidez principalmente sobre a costa sul do canal, gerando um delta de fluxo com bancos alargados na direção das correntes de maré. As plumas de turbidez permitiram identificar padrões gerais de circulação da maré.
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spelling doaj.art-89e8f33c33bc4df8ae5ebce8eb2042b72022-12-21T19:10:01ZengUniversidade de São PauloBrazilian Journal of Oceanography1679-87591982-436X2011-09-0159324125210.1590/S1679-87592011000300004Study of the surface water circulation in San Blas channel (Argentina) using landsat imageryDébora BeigtDiana G. CuadradoMaría C. PiccoloThis paper deals with the application of satellite images to study turbidity and water circulation patterns in San Blas channel during a theoretical tidal cycle. Eight Landsat TM and ETM images acquired under clear-sky conditions and representing different tidal stages were selected from a pool of Landsat images provided by the argentinean National Commission of Space Activities (CONAE) and the US Geological Survey. Standard digital image processing techniques were used to perform geometric and radiometric corrections on the visible and near-infrared bands. An image-based atmospheric correction (COST method by CHAVEZ, 1996) was applied. An ISODATA unsupervised classification was performed in order to identify different turbidity levels throughout the channel and adjacent areas. The results suggest that suspended sediment transport towards the channel mouth by ebb currents occurs along both flanks. These currents carry suspended sediment into the open sea, generating an ebb tidal delta which tends to rotate in a clockwise direction. Flood currents trigger turbidity mostly over the southern flank of the channel, generating a flood tidal delta with elongated banks extending in the direction of the tidal currents. From the elongated shape of the turbidity plumes, general tidal circulation patterns were identified.<br>Este trabalho analisa a turbidez e a circulação da agua no canal San Blas durante um ciclo de maré teórico através de imagens satelitais. Foram utilizadas 8 imagens Landsat TM e ETM adquiridas em condições de céu claro e ao longo de diferentes momentos da maré. As imagens foram proporcionadas pela Comisión Nacional de Actividades Espaciales (CONAE) y pelo Serviço Geológico dos Estados Unidos (USGS). As correções geométricas e radiométricas foram realizadas nas bandas do espectro visível e do infravermelho próximo, utilizando técnicas padrões de processamento digital. Foi aplicada a correção atmosférica COST (CHAVEZ, 1996). Foi realizada uma classificação ISODATA não supervisionada para identificar diferentes níveis de turbidez al longo do canal e zonas adjacentes. Os resultados sugerem que o transporte de sedimento em suspensão para a boca do canal se da ao longo de ambos flancos, pela ação das correntes de refluxo. Estas correntes geram um delta de refluxo com uma tendência de rotação para a direção sul. As correntes de fluxo provocam turbidez principalmente sobre a costa sul do canal, gerando um delta de fluxo com bancos alargados na direção das correntes de maré. As plumas de turbidez permitiram identificar padrões gerais de circulação da maré.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1679-87592011000300004TurbidezCirculação da águaImagens LandsatCanal San BlasTurbidityWater circulationLandsat imagerySan Blas channel
spellingShingle Débora Beigt
Diana G. Cuadrado
María C. Piccolo
Study of the surface water circulation in San Blas channel (Argentina) using landsat imagery
Brazilian Journal of Oceanography
Turbidez
Circulação da água
Imagens Landsat
Canal San Blas
Turbidity
Water circulation
Landsat imagery
San Blas channel
title Study of the surface water circulation in San Blas channel (Argentina) using landsat imagery
title_full Study of the surface water circulation in San Blas channel (Argentina) using landsat imagery
title_fullStr Study of the surface water circulation in San Blas channel (Argentina) using landsat imagery
title_full_unstemmed Study of the surface water circulation in San Blas channel (Argentina) using landsat imagery
title_short Study of the surface water circulation in San Blas channel (Argentina) using landsat imagery
title_sort study of the surface water circulation in san blas channel argentina using landsat imagery
topic Turbidez
Circulação da água
Imagens Landsat
Canal San Blas
Turbidity
Water circulation
Landsat imagery
San Blas channel
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1679-87592011000300004
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AT dianagcuadrado studyofthesurfacewatercirculationinsanblaschannelargentinausinglandsatimagery
AT mariacpiccolo studyofthesurfacewatercirculationinsanblaschannelargentinausinglandsatimagery