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Radar Rainfall Estimation of a Severe Thunderstorm over Jeddah

Radar Rainfall Estimation of a Severe Thunderstorm over Jeddah

作     者:Ayman Mohammed Hashem Albar Abdulrahman Khalaf AL-Khalaf Heshmat Abdel-Basset Mohamed 

作者机构:Presidency of Meteorology and Environment Jeddah Kingdom of Saudi Arabia Department of Meteorology Faculty of Meteorology Environment and Arid Land Agriculture King Abdulaziz University Jeddah Kingdom of Saudi Arabia Department of Astronomy and Meteorology Faculty of Science Al-Azhar University Cairo Egypt 

出 版 物:《Atmospheric and Climate Sciences》 (大气和气候科学(英文))

年 卷 期:2015年第5卷第3期

页      面:302-316页

学科分类:1002[医学-临床医学] 100214[医学-肿瘤学] 10[医学] 

主  题:Rainfall Radar Reflectivity Z-R relationship Buffer Spatial GIS Jeddah Flood Saudi Arabia 

摘      要:The regular occurrence of flash floods over the region of Jeddah, Saudi Arabia in the past decade has highlighted the serious need for the development of early warning systems. Radar stations have been installed in Jeddah in the last decade whose active radius covers the Middle Western area of the country. Therefore, radar information and the associated the rainfall estimates are potentially useful components of an effective early warning system. Weather radar can potentially provide high-resolution spatial and temporal rainfall estimates that bring more accuracy to flood warnings as well as having applications in areas with insufficient rainfall stations coverage. Weather radar does not measure rainfall depth directly. An empirical relationship between reflectivity (Z) and rainfall rate (R), called the Z-R relationship (Z = ARb), is generally used to assess the rainfall depth. In this study, the rainfall events during August-September 2007 were analyzed to develop a Z-R relationship using the Spatial Probability Technique (SPT). This technique is based on a basic GIS function and the probability matching method. Using this technique, the Z-R pairs can be analyzed for both linear and empirical power relationships. It is found that the empirical power function is more appropriate to describe Z-R relationship than a linear function for the studied area. The method is applied with some success to the flooding event of November 25, 2009. However, the investigation of the Z-R relationship is only one step in the development of a warning system;further study of other parameters relevant to rainfall and flash flood occurrence is needed.

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