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Performance and Applicability of Satellite Rainfall Estimation in Nepal

机译:尼泊尔卫星降雨估计的性能与适用性

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@@ 1. Introduction Owing to t he monsoon precipitation, diverse geological settings and r ugged terrain, Nepal is prone to flood and Iandslides. Ma ny lives and properties worth m illions of dollars are destroy ed. The monsoon season in Nepal occurs between Jun e and Septem ber; monsoon is the dominant rainfall season, with 80% of the annual rainfall occurring in that period. Based on 20 years of data (1980-2000), Nepal is found to have high vulnerability of flood disasters as reported in the UNDP global report on reducing disaster risk (UNDP 2004). Between 1983 and 2005, on average 309 people lost their lives in Nepal, due to floods and landslides that accounting for over 60% of those who died due to different types of disasters in the country. (Khanal et al, 2007) The high level of poverty and rate of po pulation gr owth has furt her increased the vul nerability to flood and landslides. Reliable weather forecasting systems are one of the most effective way s to m inimize the loss of life property. Accurate r ainfall esti mations are e ssential for reliable and timely wea ther forecasting and waming. In many countries weather forecasting has been relied upon by a dense network of rain gauge or ground based rainfall measuring radars that report in real time. In Nepal, like many other developing countries, the hydrom eteorological station networks are sparse and rainfall data are available only after a significan t delay . According to t he Department of Hydrology and Meteorology (DHM) of Nepal, the country average density is one gauge for about 33 I km2 and is especially very sparse in mountainous areas. Owing to the limited spatial coverage of ground base gauges, unavailability of real-ti me rainfall data and constraint in technical and financial resources operational flood forecasting is y et to be initiated. Precipitation is highly variable in both space and tim e and i s an im portant input in r ainfall-runoffm odeling. The availability of global coverage of satellite da to o ffers effectiv e and economical means of calculating areal rainfall estimates in sp arsely gauged areas (Artan et al., 2007b). Thus, satellite rainfall estimates (RFEs) may be one of the best and appropriate approaches for Nepal to p redict and forecast rainfall-induced runoff that may produce flooding.
机译:@@ 1.介绍由于季风降水,不同的地质环境和r ugged地形,尼泊尔容易发生洪水和Iandslides。 MA NY的生活和物业价值和数量的美元兑换美元摧毁。尼泊尔的季风季节发生在Jun E和Septem Ber之间;季风是占优势的降雨季节,在此期间发生了80%的年度降雨量。基于20年的数据(1980-2000),尼泊尔被发现在开发计划署全球关于减少灾害风险的全球报告(开发计划署2004年)中报告的洪水灾害的高脆弱性。 1983年至2005年间,平均309人在尼泊尔失去了生命,由于洪水和山体滑坡,占该国不同类型的灾害所死亡的60%以上。 (Khanal等,2007)高水平的贫困和PO Pulation Gr Owth的速度已经让她增加了洪水和山体滑坡的普遍不合症。可靠的天气预报系统是M的最有效的方法之一,以造成寿命损失。精确的R AInfall esti Mations是可靠和及时的预测和争论的E SUSE。在许多国家,天气预报已经被一系列雨量计或基于地面的降雨量测量雷达所依赖的天气预报。在尼泊尔,与其他许多其他发展中国家一样,水液站驻地网络是稀疏的,降雨数据只有在意义的T延迟之后可用。据尼泊尔水文和气象系(DHM)的说法,国家平均密度为约33毫米的规格,山区尤为稀少。由于地面基座仪表的空间覆盖率有限,Real-Ti Me降雨数据和技术和财务资源运营洪水预测的限制是y eT的降雨数据和约束。在空间和Tim E中,降水在R Ainfall-Runoffm Oreeling中是高度变化的。全球卫星da的可用性覆盖到o ffers efffectiv e和计算SP的面积降雨估计的经济方法(Artan等,2007b)。因此,卫星降雨估计(RFE)可以是尼泊尔的最佳和适当方法之一,其降雨和预测可能产生洪水的降雨诱导的径流。

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