检索结果-南通市图书馆

Diagnosis of the Causes of the Rain Flooding in June in the West Africa Coastal Area

Atmospheric and Climate Sciences 2021年第1期11卷 11-31页

作者： Joël Amouin Kouassi Yves Kouadio Modeste Kacou sandrine djakouré Samuel Ta Laboratory of Matter Environmental and Solar Energy Sciences (LASMES) Ocean-Atmosphere Interaction Group University F.H.B. of Cocody Abidjan Abidjan C&ocirc te d’Ivoire Abidjan Meteorological Center of the Agency for the Safety of Air Navigation in Africa and Madagascar (ASECNA) Abidjan C&ocirc te d’Ivoire

Rain flooding during June on the West Africa coastal area is analyzed by using the 95th and 75th percentiles, which represent extreme and intense rainfall events respectively. Thus, the contribution of these events that reaches around 50% shows their impact on the rainfall in June. Atmospheric and oceanic factors influence the rain flooding. Indeed, the extreme events are associated with easterly waves propagating from 20°E, while those of intense events are initiated around 5°E. The impact of oceanic conditions exhibits the warming of the equatorial rail and the Atlantic cold tongue, the warming of the whole ocean basin and a north-south dipole of SST anomalies. The West African monsoon that reaches Abidjan corresponds to a low-level atmospheric flow, whose upward motion extends in latitude from the ocean to the continent. An increase of disturbance contributes to enhancing these events. This is confirmed by the inflow on to the continent of oceanic moisture coming from the ventilation by evaporation of warm water. In addition, the coupled ocean-atmosphere simulations are one of the best candidates that could help to better explain these dramatic events. This study is useful because of showing solutions that could help in adoption of policies for the risks management related to these events.

关键词： West Africa Coast Rain Flooding Threshold Atmospheric and Ocean Surface Conditions

来源：

维普期刊数据库评论

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

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

引用

Open Journal of Marine Science 2024年第4期14卷 63-77页

作者： 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

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

来源：

维普期刊数据库评论

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

Influence of Continental Atmospheric Forcing on the Decadal Variability of the West African Monsoon

引用

Atmospheric and Climate Sciences 2024年第1期14卷 1-28页

作者： Adjoua Moïse Landry Famien sandrine djakouré Bi Tra Jean Claude Youan Serge Janicot Abé Delfin Ochou Arona Diedhiou Département des Sciences et Techniques Université Alassane Ouattara de Bouaké Bouaké C&#244te d’Ivoire LASMES-UFR SSMT Université Félix Houphou&#235t Boigny d’Abidjan Abidjan C&#244te d’Ivoire LSS-UFR SSMT Université Félix Houphou&#235t Boigny d’Abidjan Abidjan C&#244te d’Ivoire Laboratoire d’Océanographie et du Climat: Expérimentations et Approches Numériques Sorbonne Université IRD CNRS MNHN Paris France Université Grenoble Alpes IRD CNRS Grenoble INP IGE Grenoble France UFHB-IRD Joint International Laboratory of Research on NEXUS Climate Water Energy and Agriculture and Development of Cli-mate Services African Centre of Excellence CCBAD (Climate Change Biodiversity and Sustainable Agriculture) Université Félix Houphou&#235t-Boigny Abidjan C&#244te D’Ivoire

The West African Monsoon (WAM) is characterized by strong decadal and multi-decadal variability and the impacts can be catastrophic for the local populations. One of the factors put forward to explain this variability involves the role of atmospheric dynamics, linked in particular to the Saharan Heat Low (SHL). This article addresses this question by comparing the sets of preindustrial control and historical simulation data from climate models carried out in the framework of the CMIP5 project and observations data over the 20th century. Through multivariate statistical analyses, it was established that decadal modes of ocean variability and decadal variability of Saharan atmospheric dynamics significantly influence decadal variability of monsoon precipitation. These results also suggest the existence of external anthropogenic forcing, which is superimposed on the decadal natural variability inducing an intensification of the signal in the historical simulations compared to preindustrial control simulations. We have also shown that decadal rainfall variability in the Sahel, once the influence of oceanic modes has been eliminated, appears to be driven mainly by the activity of the Arabian Heat Low (AHL) in the central Sahel, and by the structure of the meridional temperature gradient over the inter-tropical Atlantic in the western Sahel.

关键词： Influence of Continental Atmospheric Forcing on the Decadal Variability of the West African Monsoon

来源：

维普期刊数据库评论

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

Effects of Natural Processes on Sea Level Change along the West African Coastline

引用

Open Journal of Marine Science 2024年第4期14卷 78-95页

作者： Anoumou R. Tano sandrine djakouré Kouamé J. Koffi Yves Kouadio Yao Tchetche Donatus B. Angnuureng Angora Aman François-Xavier B. D. Bouo Appeaning Addo Laboratory of Fundamental and Applied Physics Nangui Abrogoua University Abidjan Cote dIvoire Laboratory of Sciences of Matter Environment and Solar Energy Felix Houphoet Boigny University of Cocody Abidjan Cote dIvoire Laboratory of Physics University of Man Man Cote dIvoire Africa Centre of Excellence in Coastal Resilience University of Cape Coast Cape Coast Ghana Department of Marine and Fisheries Sciences University of Ghana Accra Ghana

Coastal hazards induced by meteo-marine forcing are exacerbated by sea level change along the West African coastline. Changes in sea level are induced by ocean processes such as ocean heat content and river discharge. However, although these processes control largely change in sea level, they remain poorly understood. This study analyzes changes in ocean heat content, river discharge, and sea level and establishes an interconnection between these parameters using several statistical methods over the 1993-2021 period. Results showed a significant correlation between sea level and ocean heat content at 2000 m depth. The yearly minimum value appears in July from Cote d’Ivoire to Benin, whilst this value appears in June in Nigeria. The temporal variability of ocean heat content, river discharge and sea level along the West African coastline exhibits three or four periods interrupted by some breakpoints with unequal duration. The results indicate that the 1993-2000 period was dominated by an increasing ocean heat content along the coastline, while the period after the 2000s exhibits mostly a decreasing trend. Positive and negative trends characterized river discharge and sea level along this coastline. The result of multiple linear regression between sea level, river discharge and ocean heat content is a good approximation of sea level trend along the West African coastline. The results of this study could be used to predict future sea level trends along the coast.

关键词： Coastal Sea Level River Discharge Heat Content West African Coast

来源：

维普期刊数据库评论

在线全文

维普期刊数据库

学校读者我要写书评

暂无评论

欢迎您,

建议与咨询留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

时间限定

文献类型

馆藏选择

核心期刊

语言

文献类型

帮助

文字说明：

检索规则说明：

检索范例：

分类表

所选分类

限定检索结果

文献类型

馆藏范围

日期分布

学科分类号

主题

机构

作者

语言

在线全文

在线全文

在线全文

在线全文

请选择保存的检索档案：

请选择收藏分类：

通借通还

欢迎您,

建议与咨询 留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

时间限定

文献类型

馆藏选择

核心期刊

语言

文献类型

帮助

文字说明：

检索规则说明：

检索范例：

分类表

所选分类

限定检索结果

文献类型

馆藏范围

日期分布

学科分类号

主题

机构

作者

语言

在线全文

在线全文

在线全文

在线全文

请选择保存的检索档案： 新增检索档案 确定 取消

请选择收藏分类： 新增自定义分类 确定 取消

通借通还

建议与咨询留下您的常用邮箱和电话号码，以便我们向您反馈解决方案和替代方法

请选择保存的检索档案：

请选择收藏分类：