Offshore wave climate of the Pará-Maranhão Basin, Amazonian continental shelf

Abstract This study assesses the offshore wave climate of the Pará-Maranhão Basin on the Amazonian continental shelf, a crucial region for its environmental and economic activities, including fishing and extractive activities, potential oil exploration, and complex landscape marked by extensive mangrove systems comprising protected areas and touristic coastal cities in an accelerated stage of development that face significant challenges with coastal erosion. Despite the region’s relevance, studies on wave climate are scarce. To address this gap, this research provides a detailed assessment of the offshore wave climate of the North Brazilian Coast, particularly the Pará-Maranhão sector. This quantitative assessment allowed a comprehensive characterization of the wave climate in the region. Such detailed understanding is essential for various stakeholders involved in coastal management, marine transportation and environmental protective initiatives. To do so, long-term (27-year) datasets of wave parameters (Hs, Tp, DirTp) were analyzed by bivariate histograms, using WAVERYS model, which after an in-depth comparison with ERA-5 and WW3 was found to represent local wave conditions most accurately. The study’s results also showed the greatest joint occurrence of waves is observed when peak periods vary between six and eight seconds, predominantly originating from the east-northeast (ENE) to the east-southeast (ESE) directions (local wind-generated waves associated with trade winds), accounted for approximately 41% of occurrences, with higher occurrences from E (25%). Additionally, waves with peak periods longer than 20 seconds predominantly originate from directions spanning north-northeast (NNE) to east-northeast (ENE) (swell waves from the Northern Hemisphere). Moreover, this study holds the promise for replication in other regions with similar data constraints and can contribute to the future implementation of a refraction-diffraction model, essential for the design of coastal infrastructures. Thus, subsidizing informed decision-making for sustainable coastal development in the Amazon littoral.

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Publication Details

Journal
Ocean and Coastal Research
Published
2025-01-01
DOI
https://doi.org/10.1590/2675-2824073.23129
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
Field-Weighted Citation Impact
0.00

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article

Offshore wave climate of the Pará-Maranhão Basin, Amazonian continental shelf

João Luiz Baptista de Carvalho, Henrique P. P. Pereira, Susana B. Vinzón, Eduardo Vitarelli de Queiroz et al.
Ocean and Coastal Research
Oceanographic and Atmospheric Processes
article

Offshore wave climate of the Pará-Maranhão Basin, Amazonian continental shelf

João Luiz Baptista de Carvalho, Henrique P. P. Pereira, Susana B. Vinzón, Eduardo Vitarelli de Queiroz, Inaiê Malheiros Miranda, Juliana de Sá Guerreiro
article en

Abstract

Abstract This study assesses the offshore wave climate of the Pará-Maranhão Basin on the Amazonian continental shelf, a crucial region for its environmental and economic activities, including fishing and extractive activities, potential oil exploration, and complex landscape marked by extensive mangrove systems comprising protected areas and touristic coastal cities in an accelerated stage of development that face significant challenges with coastal erosion. Despite the region’s relevance, studies on wave climate are scarce. To address this gap, this research provides a detailed assessment of the offshore wave climate of the North Brazilian Coast, particularly the Pará-Maranhão sector. This quantitative assessment allowed a comprehensive characterization of the wave climate in the region. Such detailed understanding is essential for various stakeholders involved in coastal management, marine transportation and environmental protective initiatives. To do so, long-term (27-year) datasets of wave parameters (Hs, Tp, DirTp) were analyzed by bivariate histograms, using WAVERYS model, which after an in-depth comparison with ERA-5 and WW3 was found to represent local wave conditions most accurately. The study’s results also showed the greatest joint occurrence of waves is observed when peak periods vary between six and eight seconds, predominantly originating from the east-northeast (ENE) to the east-southeast (ESE) directions (local wind-generated waves associated with trade winds), accounted for approximately 41% of occurrences, with higher occurrences from E (25%). Additionally, waves with peak periods longer than 20 seconds predominantly originate from directions spanning north-northeast (NNE) to east-northeast (ENE) (swell waves from the Northern Hemisphere). Moreover, this study holds the promise for replication in other regions with similar data constraints and can contribute to the future implementation of a refraction-diffraction model, essential for the design of coastal infrastructures. Thus, subsidizing informed decision-making for sustainable coastal development in the Amazon littoral.

Ocean and Coastal ResearchVol. 73
Universidade Federal do Rio de Janeiro (BR), Universidade Federal do Maranhão (BR), Universidade Federal do Pará (BR)
Fundação Amazônia Paraense de Amparo à Pesquisa, Fundação Amparo e Desenvolvimento da Pesquisa
Openalex Percentile: Top 90%
Oceanographic and Atmospheric Processes
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