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Evaluation of satellite rainfall estimates over the Lake Tana basin at the source region of the Blue Nile River

机译:青尼罗河源区塔纳湖流域卫星降雨估算的评估

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摘要

Satellite rainfall estimates (SREs) have become alternative sources of rainfall data for several applications. However, the accuracy of the SREs is likely to vary from region to region and must be evaluated on a local basis. This study evaluated the accuracy of three SREs for the Lake Tana basin in northwestern Ethiopia. This basin is characterized by complex topography comprising both lowlands and highlands. The three SREs were the Tropical Applications of Meteorology using SATellite data and ground-based observations (TAMSAT), the Climate Hazard Infrared Precipitation with Stations (CHIRPS), and the Africa Rainfall Climatology (ARC). The SREs were compared with gauge measurements in lowland and highland regions during the period 1995-2010 on a point-to-pixel basis at daily, dekadal (10 days), monthly, and seasonal periodicities. The results show that the three SREs underestimated rainy events, but TAMSAT captured rainfall occurrence relatively well in both regions. ARC better estimated light rain rates (1-5 mm d(-1)) than did TAMSAT and CHIRPS; however, all the SREs markedly underestimated moderate and heavier rain rates (= 10 mm d(-1)). TAMSAT and CHIRPS estimated the amount of rainfall reasonably well (high efficiency, low random errors, and bias 10%) at daily, dekadal, and monthly time scales, whereas ARC did not perform satisfactorily (high random errors, low efficiency, and bias 20%) at any time scale. On a seasonal scale, CHIRPS estimated the secondary rainy season (March-May) rainfall better than did ARC and TAMSAT, whereas TAMSAT outperformed both CHIRPS and ARC during the primary rainy season (June-September). Overall, the rainfall detection capabilities and rainfall amount estimates of the SREs were better over the lowlands, and the cumulative rainfall estimates tended to improve with increasing integration time (i.e., from daily to seasonal totals).
机译:卫星降雨量估算(SRE)已成为几种应用的替代降雨数据来源。但是,SRE的准确性可能因地区而异,必须在本地进行评估。这项研究评估了埃塞俄比亚西北部塔纳湖盆地三个SRE的准确性。该盆地的特征是包括低地和高地的复杂地形。这三个SRE是使用SATellite数据和地面观测(TAMSAT)进行的气象学在热带中的应用,带站的气候灾害红外降水(CHIRPS)和非洲降雨气候学(ARC)。在1995-2010年期间,将SRE与低地和高地地区的测量值进行了比较,以点,像素为基础,逐日,十度(10天),每月和季节性周期性。结果表明,三个SRE低估了降雨事件,但TAMSAT较好地捕获了两个地区的降雨事件。 ARC比TAMSAT和CHIRPS更好的估计小雨率(1-5 mm d(-1));但是,所有的SRE明显低估了中等和较大的降雨率(> = 10 mm d(-1))。 TAMSAT和CHIRPS估计在每日,十度和每月时间尺度上的降雨量相当好(高效率,低随机误差和偏差<10%),而ARC表现不令人满意(高随机误差,低效率和偏差) > 20%)。在季节尺度上,CHIRPS估计次雨季(3月至5月)的降雨量要好于ARC和TAMSAT,而TAMSAT在主要雨季(6月至9月)的表现均优于CHIRPS和ARC。总体而言,SRE的降雨探测能力和降雨量估算值在低地上更好,并且累积降水量估算值随着积分时间的增加而趋于改善(即从每日到季节性总量)。

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