2014
DOI: 10.1590/s2179-975x2014000200010
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Morphological characterization of eighteen lakes of the north and middle coast of Rio Grande do Sul, Brazil

Abstract: Aims: The present study aimed at a morphological characterization of 18 lakes of the municipalities of Cidreira, Balneário Pinhal and Palmares do Sul, situated in the northern and middle coastal plain of Rio Grande do Sul, Brazil. Methods: The morphometric survey was conducted in the summer of 2011/2012, based on echo sounder coupled with GPS and the application of remote sensing and GIS procedures. The morphometric parameters used for the characterization were: surface area, perimeter, perimeter development, … Show more

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Cited by 10 publications
(10 citation statements)
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References 17 publications
(19 reference statements)
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“…Changes in lakes can be manifested in surface area, volume or capacity changes and variation in the water quality depending on the dynamics in the contributing area, the size and shape of the water body, and the geologic formation. The study of lake morphology is important not only to understand spatial change in the shape and size of the lake, but also to comprehend its hydrologic and limnologic characteristics [5][6][7]. Historical morphometric studies in general provide information on spatial and temporal changes in erosion and sediment deposition, as well as bathymetric characteristics.…”
Section: Introductionmentioning
confidence: 99%
“…Changes in lakes can be manifested in surface area, volume or capacity changes and variation in the water quality depending on the dynamics in the contributing area, the size and shape of the water body, and the geologic formation. The study of lake morphology is important not only to understand spatial change in the shape and size of the lake, but also to comprehend its hydrologic and limnologic characteristics [5][6][7]. Historical morphometric studies in general provide information on spatial and temporal changes in erosion and sediment deposition, as well as bathymetric characteristics.…”
Section: Introductionmentioning
confidence: 99%
“…The number and distribution of transects, and number of depth points per square kilometer (8,857) used for generating the bathymetric chart seemed satisfactory for a detailed representation of bottom contour, as compared to similar surveys in Carioca Lake (7,843 points.km 2 ) (Bezerra-Neto et al, 2010) and Umari and Santa Cruz Reservoirs (respectively 1,812 and 1,895 points.km 2 ) (Moura et al, 2015). Schäfer et al, 2014;Silva et al, 2018;b. Fantin-Cruz et al, 2008;c.…”
Section: Discussionmentioning
confidence: 99%
“…Surface area (A) and areas at each 1-m isobath were used for the estimation of volume (V) and for the hypsographic curves of depth-area and depth volume, according to Wetzel & Likens (2000). The morphometric parameters mean depth (Z), relative depth (Zr) and shore line development index (DL) followed Wetzel & Likens (2000), the development volume index (Dv) was calculated according to Schäfer (1984), and the mean width according to Wetzel (2001).…”
Section: Data Analysis and Morphometric Parameters Estimationmentioning
confidence: 99%
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“…The study area covers >100 freshwater lakes of variable sizes (from 0.01 up to 10,000 km 2 ) (Schwarzbold & Schäfer, 1984). The coastal lakes selected are shallow (usually <10 m deep (Schäfer et al, 2009(Schäfer et al, , 2014(Schäfer et al, , 2017 and subject to strong and regular winds, which promote circulation and resuspension of bottom sediments, and influence nutrients balance, eutrophication rate and siltation, resulting in highly dynamic lake ecosystems with varying eutrophication states (Schäfer et al, 2014(Schäfer et al, , 2017.…”
Section: Study Area and Study Sitesmentioning
confidence: 99%