Relationship between the Guinea Current and the Coastal Upwelling in Northern of Gulf of Guinea  

作　　者：Sandrine Djakouré Youssouf Konaté Vamara Koné Kouacou Bosson Mamadou Koné Kouassi Yves Kouadio Sandrine Djakouré;Youssouf Konaté;Vamara Koné;Kouacou Bosson;Mamadou Koné;Kouassi Yves Kouadio(Laboratory of Matter Sciences, Environment and Solar Energy (LASMES), University Felix Houphouet Boigny of Cocody-Abidjan, Abidjan, Cte dIvoire;UFR of Marine Sciences, University of San-Pdro, San-Pdro, Cte dIvoire;Laboratory of Environmental Sciences and Techniques (LSTE), University Jean-Lorougnon Gud, Daloa, Cte dIvoire)

机构地区：[1]Laboratory of Matter Sciences, Environment and Solar Energy (LASMES), University Felix Houphouet Boigny of Cocody-Abidjan, Abidjan, Cte dIvoire [2]UFR of Marine Sciences, University of San-Pdro, San-Pdro, Cte dIvoire [3]Laboratory of Environmental Sciences and Techniques (LSTE), University Jean-Lorougnon Gud, Daloa, Cte dIvoire

出　　处：《Open Journal of Marine Science》2024年第4期63-77,共15页海洋科学期刊（英文）

摘　　要：The variability of ocean circulation and sea surface temperature (SST) in the tropical Atlantic, especially in the Gulf of Guinea (GG), defines this region as exceptionally rich from an oceanographic perspective. The Guinea Current (GC), as the major surface current, plays a significant role in marine productivity and coastal upwelling in the GG. This coastal upwelling is known to influence the climate of the surrounding region, primary productivity and local fisheries. Studies on GC variability and its impact on this coastal upwelling have highlighted that the upwelling downstream of Cape Palmas is influenced by GC detachment, topographic variations and advective processes leading to significant vertical mixing. This study aims to analyze the interannual variability of the GC and its impact on coastal upwelling using the Coastal and Regional Ocean COmmunity model (CROCO). The model’s evaluation is conducted using observational data, specifically Geostrophic and EKman Current Observatory (GEKCO) and Ocean Surface Current Analysis (OSCAR) for currents, and Air-sea Fluxes for the global Tropic ocean-description (TROPFLUX) and Optimum Interpolation-Sea Surface Temperature (OI-SST) for temperature. Thus, the model evaluation indicates that it accurately replicates ocean circulation and SST patterns in the tropical Atlantic and the GG. The joint analysis of upwelling indices (surface and intensity) and the position of the GC core allowed us to conclude that the displacement of the GC core does indeed influence the upwelling indices in the northern part of GG. However, other oceanic and atmospheric mechanisms such as vertical diffusion and horizontal advection as proposed by previous studies may also affect the year-by-year variability of coastal upwelling in the northern GG.The variability of ocean circulation and sea surface temperature (SST) in the tropical Atlantic, especially in the Gulf of Guinea (GG), defines this region as exceptionally rich from an oceanographic perspective. The Guinea Current (GC), as the major surface current, plays a significant role in marine productivity and coastal upwelling in the GG. This coastal upwelling is known to influence the climate of the surrounding region, primary productivity and local fisheries. Studies on GC variability and its impact on this coastal upwelling have highlighted that the upwelling downstream of Cape Palmas is influenced by GC detachment, topographic variations and advective processes leading to significant vertical mixing. This study aims to analyze the interannual variability of the GC and its impact on coastal upwelling using the Coastal and Regional Ocean COmmunity model (CROCO). The model’s evaluation is conducted using observational data, specifically Geostrophic and EKman Current Observatory (GEKCO) and Ocean Surface Current Analysis (OSCAR) for currents, and Air-sea Fluxes for the global Tropic ocean-description (TROPFLUX) and Optimum Interpolation-Sea Surface Temperature (OI-SST) for temperature. Thus, the model evaluation indicates that it accurately replicates ocean circulation and SST patterns in the tropical Atlantic and the GG. The joint analysis of upwelling indices (surface and intensity) and the position of the GC core allowed us to conclude that the displacement of the GC core does indeed influence the upwelling indices in the northern part of GG. However, other oceanic and atmospheric mechanisms such as vertical diffusion and horizontal advection as proposed by previous studies may also affect the year-by-year variability of coastal upwelling in the northern GG.

关 键 词：Guinea Current Sea Surface Temperature Coastal Upwelling Gulf of Guinea Tropical Atlantic Ocean 

分 类 号：P73[天文地球—海洋科学]