Brazil Wave Climate from a High-Resolution Wave Hindcast
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)...
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MDPI AG
2022
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Online Access: | https://doi.org/10.3390/cli10040053 https://doaj.org/article/6d5beca337be45a094e6e6db0f6bf0c4 |
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ftdoajarticles:oai:doaj.org/article:6d5beca337be45a094e6e6db0f6bf0c4 2023-05-15T17:33:55+02:00 Brazil Wave Climate from a High-Resolution Wave Hindcast Camila de Sa Cotrim Alvaro Semedo Gil Lemos 2022-03-01T00:00:00Z https://doi.org/10.3390/cli10040053 https://doaj.org/article/6d5beca337be45a094e6e6db0f6bf0c4 EN eng MDPI AG https://www.mdpi.com/2225-1154/10/4/53 https://doaj.org/toc/2225-1154 doi:10.3390/cli10040053 2225-1154 https://doaj.org/article/6d5beca337be45a094e6e6db0f6bf0c4 Climate, Vol 10, Iss 53, p 53 (2022) wave analysis ERA5 South Atlantic Ocean Science Q article 2022 ftdoajarticles https://doi.org/10.3390/cli10040053 2022-12-31T00:32:44Z 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 Directory of Open Access Journals: DOAJ Articles Southern Ocean Climate 10 4 53 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
wave analysis ERA5 South Atlantic Ocean Science Q |
spellingShingle |
wave analysis ERA5 South Atlantic Ocean Science Q Camila de Sa Cotrim Alvaro Semedo Gil Lemos Brazil Wave Climate from a High-Resolution Wave Hindcast |
topic_facet |
wave analysis ERA5 South Atlantic Ocean Science Q |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Camila de Sa Cotrim Alvaro Semedo Gil Lemos |
author_facet |
Camila de Sa Cotrim Alvaro Semedo Gil Lemos |
author_sort |
Camila de Sa Cotrim |
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 AG |
publishDate |
2022 |
url |
https://doi.org/10.3390/cli10040053 https://doaj.org/article/6d5beca337be45a094e6e6db0f6bf0c4 |
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, Vol 10, Iss 53, p 53 (2022) |
op_relation |
https://www.mdpi.com/2225-1154/10/4/53 https://doaj.org/toc/2225-1154 doi:10.3390/cli10040053 2225-1154 https://doaj.org/article/6d5beca337be45a094e6e6db0f6bf0c4 |
op_doi |
https://doi.org/10.3390/cli10040053 |
container_title |
Climate |
container_volume |
10 |
container_issue |
4 |
container_start_page |
53 |
_version_ |
1766132566513942528 |