Morphological variability of the sandspit of the Araranguá river estuary, Santa Catarina
DOI:
https://doi.org/10.22456/1807-9806.130958Keywords:
depositional environment, Remote Sensing, coastal evolution, QuaternaryAbstract
Characterization of coastal depositional systems through the use and interpretation of remote sensing data enables studies both on the surface and on the subsurface of this environment. In a scenario of global environmental changes, coastal depositional environments are one of the most vulnerable ecosystems to rising sea levels. The objective of this work was to characterize the morphological dynamics of the sandspit of the Araranguá River, in Santa Catarina, between 1984 and 2021, using multispectral satellite images on the surface of orbital optical sensors Thematic Mapper (TM)/Landsat 5, Enhanced Thematic Mapper Plus (ETM+)/Landsat 7 and Operational Terra Imager (OLI)/Landsat 8. For this, an interval of 37 years of satellite images was used, whose data were obtained from the “Earth Explorer” database of the United States Geological Survey. Digital image processing was performed using ENVI software, version 5.3. The depositional features were identified, vectored and the thematic maps were generated using ArcGIS® software, version 10.3. The morphometric data generated were tabulated, analyzed, and compared in electronic spreadsheets. The spit presents a tendency of sedimentary accretion in relation to its area and length and is in the process of progradation towards the northeast. The spit prograded approximately 3550 m in the analyzed period, and its area increased by 670 m². The average rate of progradation calculated was 98.5 m per year. The morphodynamics of the Araranguá River sandspit are conditioned by coastal overwash events, flooding, and human interventions.
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