EVALUATION OF QUALITY OF THE WAVE DATABASE OF THE COASTAL MODELING SYSTEM – BRAZIL TO THE EASTERN COAST OF BRAZIL

The purpose of the present work was to evaluate the quality of the wave database of the SMC - BRASIL program, especially regarding the existence of NE waves in a stretch of the Brazilian eastern coast. For this, modeling was performed in regions whose geomorphological indicators indicated coastal...

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Main Authors: Gabriela Amado Frutuoso, Junia Kacenelenbogen, Iracema Reimão
Format: Article
Language:Portuguese
Published: Programa de Pós-graduação em Geografia (PPGEO) 2019-07-01
Series:GeoNordeste
Subjects:
Online Access:https://seer.ufs.br/index.php/geonordeste/article/view/11246/pdf
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spelling doaj-faddffed26b740649df0fa9449d4e4ad2020-11-25T02:45:32ZporPrograma de Pós-graduação em Geografia (PPGEO)GeoNordeste1518-60592318-26952019-07-01XXX12642https://doi.org/10.33360/RGN.2318-2695.2019.i1p26-42EVALUATION OF QUALITY OF THE WAVE DATABASE OF THE COASTAL MODELING SYSTEM – BRAZIL TO THE EASTERN COAST OF BRAZILGabriela Amado Frutuoso0Junia Kacenelenbogen1Iracema Reimão2FrutuosoGuimarãesSilvaThe purpose of the present work was to evaluate the quality of the wave database of the SMC - BRASIL program, especially regarding the existence of NE waves in a stretch of the Brazilian eastern coast. For this, modeling was performed in regions whose geomorphological indicators indicated coastal drift to the SE and SO quadrants, which theoretically would be caused by these waves, in the municipalities of Ilhéus / BA, Prado / BA, and Itaúnas / ES. In the SMC database, NE waves were only identified in Prado (0.01%). ENE waves were identified in Prado (3.01%), Ilhéus (0.02%) and Itaúnas (0.02%). In all cases, the occurrences were much smaller than those recorded in wave statistics and in the literature. The coastal transport modeled for the three areas was directed to N, NE and NO, in a way contrary to the one expected by the configuration of the sand spits present. Coastal currents modeled for NE and ENE waves are directed to the SE and SO quadrants, which demonstrates that the currents generated by the program are coherent; and that the program problem is the small amount of these waves present in your database, which affects the result of the efective coastal transport.https://seer.ufs.br/index.php/geonordeste/article/view/11246/pdfLittoral DriftWave RegimeEast Coast of Brazil.
collection DOAJ
language Portuguese
format Article
sources DOAJ
author Gabriela Amado Frutuoso
Junia Kacenelenbogen
Iracema Reimão
spellingShingle Gabriela Amado Frutuoso
Junia Kacenelenbogen
Iracema Reimão
EVALUATION OF QUALITY OF THE WAVE DATABASE OF THE COASTAL MODELING SYSTEM – BRAZIL TO THE EASTERN COAST OF BRAZIL
GeoNordeste
Littoral Drift
Wave Regime
East Coast of Brazil.
author_facet Gabriela Amado Frutuoso
Junia Kacenelenbogen
Iracema Reimão
author_sort Gabriela Amado Frutuoso
title EVALUATION OF QUALITY OF THE WAVE DATABASE OF THE COASTAL MODELING SYSTEM – BRAZIL TO THE EASTERN COAST OF BRAZIL
title_short EVALUATION OF QUALITY OF THE WAVE DATABASE OF THE COASTAL MODELING SYSTEM – BRAZIL TO THE EASTERN COAST OF BRAZIL
title_full EVALUATION OF QUALITY OF THE WAVE DATABASE OF THE COASTAL MODELING SYSTEM – BRAZIL TO THE EASTERN COAST OF BRAZIL
title_fullStr EVALUATION OF QUALITY OF THE WAVE DATABASE OF THE COASTAL MODELING SYSTEM – BRAZIL TO THE EASTERN COAST OF BRAZIL
title_full_unstemmed EVALUATION OF QUALITY OF THE WAVE DATABASE OF THE COASTAL MODELING SYSTEM – BRAZIL TO THE EASTERN COAST OF BRAZIL
title_sort evaluation of quality of the wave database of the coastal modeling system – brazil to the eastern coast of brazil
publisher Programa de Pós-graduação em Geografia (PPGEO)
series GeoNordeste
issn 1518-6059
2318-2695
publishDate 2019-07-01
description The purpose of the present work was to evaluate the quality of the wave database of the SMC - BRASIL program, especially regarding the existence of NE waves in a stretch of the Brazilian eastern coast. For this, modeling was performed in regions whose geomorphological indicators indicated coastal drift to the SE and SO quadrants, which theoretically would be caused by these waves, in the municipalities of Ilhéus / BA, Prado / BA, and Itaúnas / ES. In the SMC database, NE waves were only identified in Prado (0.01%). ENE waves were identified in Prado (3.01%), Ilhéus (0.02%) and Itaúnas (0.02%). In all cases, the occurrences were much smaller than those recorded in wave statistics and in the literature. The coastal transport modeled for the three areas was directed to N, NE and NO, in a way contrary to the one expected by the configuration of the sand spits present. Coastal currents modeled for NE and ENE waves are directed to the SE and SO quadrants, which demonstrates that the currents generated by the program are coherent; and that the program problem is the small amount of these waves present in your database, which affects the result of the efective coastal transport.
topic Littoral Drift
Wave Regime
East Coast of Brazil.
url https://seer.ufs.br/index.php/geonordeste/article/view/11246/pdf
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