2009
DOI: 10.1590/s0102-261x2009000500006
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Mapeamento de ambientes costeiros tropicais (Golfão Maranhense, Brasil) utilizando imagens de sensores remotos orbitais

Abstract: ABSTRACT. This paper presents the results of coastal environmental mapping of Golfão Maranhense, Brazil, using a methodological approach that includes: (a) integrated analysis based on digital image processing of Landsat-4 TM, SPOT-2 HRV, RADARSAT-1 SAR (Synthetic Aperture Radar) and SRTM (Shuttle Radar Topography Mission) data; (b) geographic information system; (c) field surveys related to geomorphology, topography and sedimentology. Mapped environments were grouped into four sectors: Sector 1, with salt mar… Show more

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Cited by 25 publications
(15 citation statements)
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“…This marked similarity between the basins was further emphasized by the results of the BAPS analysis, with the two groups being included in a single cluster. The genetic proximity between the specimens from these two basins may be a result of their geomorphological similarities, and not least because the Pindaré is the principal tributary of the Mearim (Teixeira and Souza-Filho, 2009;Piorski, 2010).…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…This marked similarity between the basins was further emphasized by the results of the BAPS analysis, with the two groups being included in a single cluster. The genetic proximity between the specimens from these two basins may be a result of their geomorphological similarities, and not least because the Pindaré is the principal tributary of the Mearim (Teixeira and Souza-Filho, 2009;Piorski, 2010).…”
Section: Discussionmentioning
confidence: 99%
“…The Pindaré, Mearim, and Itapecuru form a group of basins typical of the region, with similar topography, and all three discharge into the Gulf of Maranhão, the Mearim/Pindaré into São Marcos Bay, and the Itapecuru in São José Bay. The lower stretches of the Itapecuru and Mearim are characterized by a distinct landscape of meanders and lakes, and the Mearim connects to the Pindaré, which is its principal tributary (Teixeira and Souza-Filho, 2009;Piorski, 2010). The geomorphological evolution of the Gulf of Maranhão reflects the fluctuations in sea level that occurred during the Pliocene and Pleistocene, which culminated in the present-day configuration of estuaries in central Maranhão (Ab'Saber, 1960).…”
Section: Introductionmentioning
confidence: 99%
“…The Coastal plateau of Maranhão spreads by a wide coastal fringe and represents a geomorphological domain that can be subdivided into four markedly differentiated sectors, according to Feitosa (2006): the moist west-northwest coast of Maranhenses Recesses, dominated by vast tidal plateaus (mangroves); its most pronounced recess, constituted by the Golfão Maranhense; the east coast, of semi-moist climate, dominated by extensive fields of moving or fixed dunes; generating, in its retro area, wide fluvialmarine plateau of extremely flat topography and practically adjusted to the level of general base, called Baixada Maranhense; and the deltaic plateau of the Parnaíba River (, Teixeira and Souza Filho, 2009;Bandeira 2013). …”
Section: Maranhense Northern Regionmentioning
confidence: 99%
“…Represented by an extensive inland plain is constituted by a seasonally flooded surface of freshwater marshes (or hydrophilic fields floodplain), intermittent lakes, halophiles fields floodplain, salt marshes (or apicuns), mangroves, muddy tidal flats (or crowns mud) and estuarine channel (Teixeira and Souza Filho, 2009), where converge the main rivers genuinely Maranhense: Itapecuru, Munim, Mearim, Grajaú and Pindaré; Typical plains river, characterized by low slope in the middle and lower stretches. It is a "Pantanal Maranhense".…”
Section: Baixada Maranhensementioning
confidence: 99%
“…Oil spill environmental sensitivity maps, adapted to the peculiarities of the Amazonian region (Souza Filho et al, 2004) were drawn at tactical scales through the use of Radarsat and Landsat sensors (Gonçalves et al, 2009;Teixeira & Souza Filho 2009;Boulhosa & Souza Filho, 2009), and operational scale through the use of High Resolution remote sensing (Andrade et al, 2010;Rodrigues & Szlafsztein 2010;Andrade et al, 2009). Over the past decade were reached advances in identification and assessment of sensitivity through spatial maps, the impacts to oil spill analyses, and oil spill risk in Amazonian coastal.…”
Section: Introductionmentioning
confidence: 99%