检索结果-南通市图书馆

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

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

Consistency in <i>Z</i>-<i>R</i>Relationship Variability Regardless Precipitating Systems, Climatic Zones Observed from Two Types of Disdrometer

引用

Atmospheric and Climate Sciences 2014年第5期4卷 941-955页

作者： Bakary Bamba abé delfin ochou Eric-Pascal Zahiri Modeste Kacou Laboratory of Atmospheric Physics and Fluid Mechanics University Félix Houphouet-Boigny Abidjan Cote d’Ivoire Geosciences Environment Toulouse (GET) University Paul Sabatier of Toulouse III Toulouse France

Data from rain Drop Size Distributions gathered on five sites in Africa as well as those of the pilot site in Kourou (French Guyana, South America), located in different climatic zones, and collected by two types of disdrometer (the impact JW RD-69 disdrometer and the Optical Spectro-Pluviometer, OSP) are used to study the consistency of the reflectivity factor-rain rate at the ground (Z-R) relationship variability. The results clearly confirm that the relationship Z-R knows a large spatial variability, from a type of precipitation to another and within the same precipitation regardless the type of disdrometer used for DSD measurements. Base on the similarity of the relations reflectivity factor-rain rate and ratio median volume diameter over the total number of drops-rain rate, the variability of the Z-R coefficients (A, b) through the simultaneously implication of the size and number of drops which characterize the DSD was exhibited. It was shown that the relationships A-α and b-β designed to understand the involvement of parameters D0 and NT of DSD in the variability of the relationship Z-R are similar regardless the types of disdrometer used. However, the relations A-α in the Sahelian region appear to deviate from those of Guinean, equatorial and Soudanian zones. The plausible reasons were discussed.

关键词： Drop Size Distributions Consistency in Z-R Relationship Variability Squall Lines Thunderstorm Stratiform Rain JW RD-69 Disdrometer Optical Spectro-Pluviometer OSP

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

Improving Radar Rainfall Estimation by Accounting for Microphysical Processes Using a Micro Rain Radar in West Africa

引用

Atmospheric and Climate Sciences 2021年第4期11卷 658-688页

作者： Ghislain Kouadio Eric-Pascal Zahiri Modeste Kacou Augustin Kadjo Koffi abé delfin ochou Paul Assamoi Laboratoire de Physique de l’Atmosphère et de Mécanique des Fluides (LAPA-MF) UFR SSMT Université Félix Houphou&#235 t-Boigny Abidjan C&#244 te d’Ivoire

This study evaluates the improvement of the radar Quantitative Precipitation Estimation (QPE) by involving microphysical processes in the determination of Z-R algorithms. Within the framework of the AMMA campaign, measurements of an X-band radar (Xport), a vertical pointing Micro Rain Radar (MRR) to investigate microphysical processes and a dense network of rain gauges deployed in Northern Benin (West Africa) in 2006 and 2007 were used as support to establish such estimators and evaluate their performance compared to other estimators in the literature. By carefully considering and correcting MRR attenuation and calibration issues, the Z-R estimator developed with the contribution of microphysical processes and non-linear least-squares adjustment proves to be more efficient for quantitative rainfall estimation and produces the best statistic scores than other optimal Z-R algorithms in the literature. We also find that it gives results comparable to some polarimetric algorithms including microphysical information through DSD integrated parameter retrievals.

关键词： Drop Distribution Micro Rain Radar Calibration Microphysical Processes Z-R Relationships Rainfall Estimation

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

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

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：