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Evaluation and comparison of four satellite-based precipitation products over the upper Tana River Basin

机译:塔纳河流域上游4种星基降水产物的评价与比较

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Abstract In developing countries, hydrological modeling in support of decision-making and planning of hydrological resources is often hindered by the scarcity of in situ hydro-meteorological data and uneven distribution of observation stations. Satellite-based precipitation products (SPPs) can potentially play a role in overcoming the challenge posed by insufficient and inconsistent in situ precipitation measurements. However, their performance in estimating observations needs to be evaluated before their application in hydrological modeling. This paper evaluates and compares four high-resolution SPPs ARC2 (African Rainfall Climatology version 2), CHIRPS (Climate Hazard Group Infrared Precipitation with Station data), TMPA 3B42v7 (Tropical Rainfall Measuring Mission Multi-satellite Precipitation Analysis 3B42 product), and PERSIANN-CDR (Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks) with measurements from rain-gauge stations (2007–2016) over the Upper Tana River Basin (UTRB). Performance of the SPPs is evaluated using continuous correlation coefficient (R), mean absolute error (MAE), root mean square error (RMSE), Nash–Sutcliffe efficiency coefficient (NSE), and percent bias (PBIAS) and categorical POD (probability of detection), FAR (false alarm ratio), CSI (critical success index), and ETS (equitable threat score) metrics at daily, dekadal, and monthly time steps. The daily, dekadal, and monthly R of ARC2 SPP were 0.8, 0.92, and 0.94, respectively. The R of CHIRPS (TMPA 3B42v7) is 0.53 (0.63), 0.82 (0.83), and 0.93 (0.95). The daily RMAEs for ARC2, CHIRPS, TMPA 3B42v7, and PERSIANN-CDR are 0.73, 1.27, 1.17, and 1.04, while the RRMSEs are 2.94, 4.52, 4.03, and 3.85, respectively. PBIAS indicates that all the SPPs except CHIRPS underestimated precipitation. It is shown that ARC2 and CHIRPS are better in reproducing the occurrence frequency of daily events for the different intensity ranges. Also, ARC2 was the best performing SPP with regard to the ability to detect precipitation events. It is observed that all SPPs were able to detect low-intensity precipitation events but poor in detecting intensity events higher than 25 mm/day. Overall, ARC2 provided the most accurate precipitation estimates, although CHIRPS and TMPA 3B42v7 also showed good performance in reproducing and detecting precipitation.
机译:摘要 在发展中国家,由于现场水文气象数据的稀缺和观测站分布不均,支持水文资源决策和规划的水文建模往往受到阻碍。基于卫星的降水产品(SPP)有可能在克服原位降水测量不足和不一致带来的挑战方面发挥作用。然而,在将其应用于水文建模之前,需要评估它们在估计观测方面的性能。本文评估和比较了四个高分辨率表面等离激元[ARC2(非洲降雨气候学第2版)、CHIRPS(气候灾害组红外降水与台站数据)、TMPA 3B42v7(热带降雨测量任务多卫星降水分析3B42产品)和PERSIANN-CDR(使用人工神经网络遥感信息进行降水估计)]与塔纳河流域上游(UTRB)雨量监测站(2007-2016)的测量结果。SPP 的性能使用连续 [相关系数 (R)、平均绝对误差 (MAE)、均方根误差 (RMSE)、Nash-Sutcliffe 效率系数 (NSE) 和百分比偏差 (PBIAS)] 和分类 [POD(检测概率)、FAR(误报率)、CSI(关键成功指数)和 ETS(公平威胁评分)] 指标在每日、十进制和每月时间步长进行评估。ARC2 SPP的日R、10dal和月R分别为0.8、0。分别为 92 和 0.94。CHIRPS (TMPA 3B42v7) 的 R 分别为 0.53 (0.63)、0.82 (0.83) 和 0.93 (0.95)。ARC2、CHIRPS、TMPA 3B42v7 和 PERSIANN-CDR 的日RMAE分别为0.73、1.27、1.17和1.04,RRMSE分别为2.94、4.52、4.03和3.85。PBIAS表明,除CHIRPS外,所有SPP都低估了降水量。结果表明,ARC2和CHIRPS在不同强度范围内均能较好地再现日事件的发生频率。此外,ARC2在检测降水事件的能力方面表现最佳。据观察,所有表面等离激元都能够检测到低强度降水事件,但在检测强度高于25 mm/d的事件方面较差。总体而言,ARC2提供了最准确的降水估计,尽管CHIRPS和TMPA 3B42v7在再现和检测降水方面也表现出良好的性能。

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