Wave Climate Variability along the Coastlines of Senegal over the Last Four Decades

Knowledge of wave climate is essential for efficient management of the world’s coastal areas. Senegal is a relevant case, given its high coastal vulnerability to energetic wave conditions. This study investigates wave climates along the coastal zone of Senegal based on a new high-resolution hindcast...

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Published in:Atmosphere
Main Authors: Marcellin Seujip Samou, Xavier Bertin, Issa Sakho, Alban Lazar, Mamadou Sadio, Mouhamadou Bachir Diouf
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/atmos14071142
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spelling ftmdpi:oai:mdpi.com:/2073-4433/14/7/1142/ 2023-08-20T04:08:26+02:00 Wave Climate Variability along the Coastlines of Senegal over the Last Four Decades Marcellin Seujip Samou Xavier Bertin Issa Sakho Alban Lazar Mamadou Sadio Mouhamadou Bachir Diouf agris 2023-07-13 application/pdf https://doi.org/10.3390/atmos14071142 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos14071142 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 14; Issue 7; Pages: 1142 wave climate WaveWatch III wave climatology wave trends remote climatic modes in situ data Atlantic Ocean Senegalese Coast Senegal Text 2023 ftmdpi https://doi.org/10.3390/atmos14071142 2023-08-01T10:51:25Z Knowledge of wave climate is essential for efficient management of the world’s coastal areas. Senegal is a relevant case, given its high coastal vulnerability to energetic wave conditions. This study investigates wave climates along the coastal zone of Senegal based on a new high-resolution hindcast covering the period 1980–2021. This study evaluates the average, seasonal, and extreme values for the significant wave heights (Hs), periods (Tm02/Tp), and mean directions (DIR). In boreal winter, the wave climate is dominated by swells coming from the North-Atlantic lows. In contrast, in boreal summer, the Southern Coast (from Dakar to Casamance) is exposed to swells generated in the South Atlantic Ocean. Throughout their refraction around the Dakar Peninsula, NW swells rotate by ~100° from NW to SW, while their Hs is roughly halved when reaching the Southern Coast of Senegal. Over the studied period, trends in Hs are weak (~0.6 cm.decade−1) on the Northern Coast and double on the Southern Coast (~1.2 cm.decade−1), mostly due to an increase during boreal summer (2 cm.decade−1). The wave periods show weak trends (~0.05 s.decade−1), and DIRs show weak counterclockwise rotation (−1°.decade−1). These trends are explained by the main climate modes of the Atlantic Ocean (NAO/EA during winter, SAM during summer) and are important for future research and long-term monitoring of the Senegalese Coast. Text North Atlantic South Atlantic Ocean MDPI Open Access Publishing Atmosphere 14 7 1142
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic wave climate
WaveWatch III
wave climatology
wave trends
remote climatic modes
in situ data
Atlantic Ocean
Senegalese Coast
Senegal
spellingShingle wave climate
WaveWatch III
wave climatology
wave trends
remote climatic modes
in situ data
Atlantic Ocean
Senegalese Coast
Senegal
Marcellin Seujip Samou
Xavier Bertin
Issa Sakho
Alban Lazar
Mamadou Sadio
Mouhamadou Bachir Diouf
Wave Climate Variability along the Coastlines of Senegal over the Last Four Decades
topic_facet wave climate
WaveWatch III
wave climatology
wave trends
remote climatic modes
in situ data
Atlantic Ocean
Senegalese Coast
Senegal
description Knowledge of wave climate is essential for efficient management of the world’s coastal areas. Senegal is a relevant case, given its high coastal vulnerability to energetic wave conditions. This study investigates wave climates along the coastal zone of Senegal based on a new high-resolution hindcast covering the period 1980–2021. This study evaluates the average, seasonal, and extreme values for the significant wave heights (Hs), periods (Tm02/Tp), and mean directions (DIR). In boreal winter, the wave climate is dominated by swells coming from the North-Atlantic lows. In contrast, in boreal summer, the Southern Coast (from Dakar to Casamance) is exposed to swells generated in the South Atlantic Ocean. Throughout their refraction around the Dakar Peninsula, NW swells rotate by ~100° from NW to SW, while their Hs is roughly halved when reaching the Southern Coast of Senegal. Over the studied period, trends in Hs are weak (~0.6 cm.decade−1) on the Northern Coast and double on the Southern Coast (~1.2 cm.decade−1), mostly due to an increase during boreal summer (2 cm.decade−1). The wave periods show weak trends (~0.05 s.decade−1), and DIRs show weak counterclockwise rotation (−1°.decade−1). These trends are explained by the main climate modes of the Atlantic Ocean (NAO/EA during winter, SAM during summer) and are important for future research and long-term monitoring of the Senegalese Coast.
format Text
author Marcellin Seujip Samou
Xavier Bertin
Issa Sakho
Alban Lazar
Mamadou Sadio
Mouhamadou Bachir Diouf
author_facet Marcellin Seujip Samou
Xavier Bertin
Issa Sakho
Alban Lazar
Mamadou Sadio
Mouhamadou Bachir Diouf
author_sort Marcellin Seujip Samou
title Wave Climate Variability along the Coastlines of Senegal over the Last Four Decades
title_short Wave Climate Variability along the Coastlines of Senegal over the Last Four Decades
title_full Wave Climate Variability along the Coastlines of Senegal over the Last Four Decades
title_fullStr Wave Climate Variability along the Coastlines of Senegal over the Last Four Decades
title_full_unstemmed Wave Climate Variability along the Coastlines of Senegal over the Last Four Decades
title_sort wave climate variability along the coastlines of senegal over the last four decades
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/atmos14071142
op_coverage agris
genre North Atlantic
South Atlantic Ocean
genre_facet North Atlantic
South Atlantic Ocean
op_source Atmosphere; Volume 14; Issue 7; Pages: 1142
op_relation Climatology
https://dx.doi.org/10.3390/atmos14071142
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos14071142
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