首页> 外文期刊>Journal of Applied Meteorology and Climatology >Rainfall Variability over Mountainous and Adjacent Lake Areas: The Case of Lake Tana Basin at the Source of the Blue Nile River
【24h】

Rainfall Variability over Mountainous and Adjacent Lake Areas: The Case of Lake Tana Basin at the Source of the Blue Nile River

机译:山区和邻近湖泊地区的降雨变化性:以青尼罗河源头的塔纳湖盆地为例

获取原文
获取原文并翻译 | 示例
           

摘要

The water resource of the Blue Nile River is of key regional importance to the northeastern African countries. However, little is known about the characteristics of the rainfall in the basin. In this paper, the authors presented the space-time variability of the rainfall in the vicinity of Lake Tana, which is the source of the Blue Nile River. The analysis was based on hourly rainfall data from a network of newly installed rain gauges, and cloud temperature indices from the Meteosat Second Generation(MSG-2) Spinning Enhanced Visible and Infrared Imager (SEVIRI) satellite sensor. The spatial and temporal patterns of rainfall were examined using not only statistical techniques such as exceedance probabilities, spatial correlation structure, harmonicanalysis, and fractal analysis but also marginal statistics such as mean and standard deviation. In addition, a convective index was calculated from remote sensing images to infer the spatial and temporal patterns of rainfall. Heavy rainfall is frequentat stations that are relatively close to the lake. The correlation distances for the hourly and the daily rainfall are found at about 8 and 18 km, respectively. The rainfall shows a strong spatially varying diurnal cycle. The nocturnal rainfall was foundto be higher over the southern shore of Lake Tana than over the mountainous area farther to the south. The maximum convection occurs between 1600 and 1700 local standard time (LST) over the Gilgel Abbay, Ribb, and Gumara catchments, and between 2200 and2300 LST over Lake Tana and the Megech catchments. In addition, the hourly rainfall of the station with the highest elevation is relatively closely clustered as compared to those stations at lower elevation. The study provides relevant information for understanding rainfall variation with elevation and distance from a lake. This understanding benefits climate and hydrological studies, water resources management, and energy development in the region.
机译:青尼罗河的水资源对东北非洲国家具有重要的区域重要性。但是,对该流域的降雨特征知之甚少。在本文中,作者介绍了塔纳湖(Blue Nile River的源头)附近降雨的时空变化。该分析基于新安装的雨量计网络的每小时降雨数据以及Meteosat第二代(MSG-2)旋转增强型可见光和红外成像仪(SEVIRI)卫星传感器的云温度指数。不仅使用统计技术(例如超标概率,空间相关结构,谐和分析和分形分析),还使用边际统计(例如均值和标准差)来检查降雨的时空格局。此外,从遥感图像计算出对流指数,以推断降雨的时空格局。相对靠近湖泊的站点经常出现大雨。每小时和每日降雨量的相关距离分别约为8 km和18 km。降雨显示强烈的空间变化的昼夜周期。塔娜湖南岸的夜间降雨高于南端的山区。最大对流发生在吉尔吉尔阿贝湾,里布和古玛拉流域上的当地标准时间(LST)1600至1700之间,塔纳湖和梅格赫流域的2200至2300 LST之间。此外,与海拔较低的站相比,海拔最高的站的小时降雨量相对接近。该研究为理解降雨随海拔和距离的变化提供了相关信息。这种了解有益于该地区的气候和水文研究,水资源管理以及能源开发。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号