Brazil Wave Climate from a High-Resolution Wave Hindcast

ABSTRACT: A detailed climatology of ocean wind waves in the South Atlantic Ocean, based on ERA-5 reanalysis and in a higher-resolution wave hindcast (ERA-5H), both developed by the European Centre for Medium-Range weather Forecasts, is presented. The higher resolution of the wave fields in the ERA-5...

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Published in:Climate
Main Authors: Cotrim, Camila De Sá, Semedo, alvaro, Lemos, Gil
Other Authors: Universidad de Cantabria
Format: Article in Journal/Newspaper
Language:English
Published: MDPI 2022
Subjects:
Online Access:http://hdl.handle.net/10902/25192
https://doi.org/10.3390/cli10040053
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spelling ftunivcantabria:oai:repositorio.unican.es:10902/25192 2023-05-15T17:33:41+02:00 Brazil Wave Climate from a High-Resolution Wave Hindcast Cotrim, Camila De Sá Semedo, alvaro Lemos, Gil Universidad de Cantabria 2022-03-31 http://hdl.handle.net/10902/25192 https://doi.org/10.3390/cli10040053 eng eng MDPI https://doi.org/10.3390/cli10040053 2225-1154 http://hdl.handle.net/10902/25192 doi:10.3390/cli10040053 © 2022 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https:// creativecommons.org/licenses/by/ 4.0/). http://creativecommons.org/licenses/by/4.0/ openAccess CC-BY Climate, 2022, 10(4), 43 Wave analysis ERA5 South Atlantic Ocean info:eu-repo/semantics/article publishedVersion 2022 ftunivcantabria https://doi.org/10.3390/cli10040053 2023-02-20T10:28:07Z ABSTRACT: A detailed climatology of ocean wind waves in the South Atlantic Ocean, based on ERA-5 reanalysis and in a higher-resolution wave hindcast (ERA-5H), both developed by the European Centre for Medium-Range weather Forecasts, is presented. The higher resolution of the wave fields in the ERA-5H (22 km) allowed for a better description of the wind sea and swell features compared to previous global and regional studies along the Brazilian coast. Overall, it is shown that swell waves are more prevalent and carry more energy in the offshore area of the study area, while wind sea waves dominate the nearshore regions, especially along the northern coast of Brazil. The influence of different climate indices on the significant wave heights patterns is also presented, with two behavioral groups showing opposite correlations to the North Atlantic Oscillation and Southern Annular Mode than to the Southern Oscillation Index. The analysis of the decadal trends of wind sea and swell heights during the ERA-5H period (1979-2020) shows that the long-term trends of the total significant wave height in the South Atlantic Ocean are mostly due to swell events and the wave propagation effect from Southern Ocean storms. Article in Journal/Newspaper North Atlantic North Atlantic oscillation South Atlantic Ocean Southern Ocean Universidad de Cantabria: UCrea Southern Ocean Climate 10 4 53
institution Open Polar
collection Universidad de Cantabria: UCrea
op_collection_id ftunivcantabria
language English
topic Wave analysis
ERA5
South Atlantic Ocean
spellingShingle Wave analysis
ERA5
South Atlantic Ocean
Cotrim, Camila De Sá
Semedo, alvaro
Lemos, Gil
Brazil Wave Climate from a High-Resolution Wave Hindcast
topic_facet Wave analysis
ERA5
South Atlantic Ocean
description ABSTRACT: A detailed climatology of ocean wind waves in the South Atlantic Ocean, based on ERA-5 reanalysis and in a higher-resolution wave hindcast (ERA-5H), both developed by the European Centre for Medium-Range weather Forecasts, is presented. The higher resolution of the wave fields in the ERA-5H (22 km) allowed for a better description of the wind sea and swell features compared to previous global and regional studies along the Brazilian coast. Overall, it is shown that swell waves are more prevalent and carry more energy in the offshore area of the study area, while wind sea waves dominate the nearshore regions, especially along the northern coast of Brazil. The influence of different climate indices on the significant wave heights patterns is also presented, with two behavioral groups showing opposite correlations to the North Atlantic Oscillation and Southern Annular Mode than to the Southern Oscillation Index. The analysis of the decadal trends of wind sea and swell heights during the ERA-5H period (1979-2020) shows that the long-term trends of the total significant wave height in the South Atlantic Ocean are mostly due to swell events and the wave propagation effect from Southern Ocean storms.
author2 Universidad de Cantabria
format Article in Journal/Newspaper
author Cotrim, Camila De Sá
Semedo, alvaro
Lemos, Gil
author_facet Cotrim, Camila De Sá
Semedo, alvaro
Lemos, Gil
author_sort Cotrim, Camila De Sá
title Brazil Wave Climate from a High-Resolution Wave Hindcast
title_short Brazil Wave Climate from a High-Resolution Wave Hindcast
title_full Brazil Wave Climate from a High-Resolution Wave Hindcast
title_fullStr Brazil Wave Climate from a High-Resolution Wave Hindcast
title_full_unstemmed Brazil Wave Climate from a High-Resolution Wave Hindcast
title_sort brazil wave climate from a high-resolution wave hindcast
publisher MDPI
publishDate 2022
url http://hdl.handle.net/10902/25192
https://doi.org/10.3390/cli10040053
geographic Southern Ocean
geographic_facet Southern Ocean
genre North Atlantic
North Atlantic oscillation
South Atlantic Ocean
Southern Ocean
genre_facet North Atlantic
North Atlantic oscillation
South Atlantic Ocean
Southern Ocean
op_source Climate, 2022, 10(4), 43
op_relation https://doi.org/10.3390/cli10040053
2225-1154
http://hdl.handle.net/10902/25192
doi:10.3390/cli10040053
op_rights © 2022 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https:// creativecommons.org/licenses/by/ 4.0/).
http://creativecommons.org/licenses/by/4.0/
openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.3390/cli10040053
container_title Climate
container_volume 10
container_issue 4
container_start_page 53
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