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首页> 外文期刊>Atmospheric research >Evaluation and comparison of CHIRPS and MSWEP daily-precipitation products in the Qinghai-Tibet Plateau during the period of 1981-2015
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Evaluation and comparison of CHIRPS and MSWEP daily-precipitation products in the Qinghai-Tibet Plateau during the period of 1981-2015

机译:1981-2015年青藏高原CHIRPS和MSWEP日降水量的评估与比较

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摘要

High-resolution, long-term and accurate daily-precipitation is always difficult and rarely measured in the Qinghai-Tibet Plateau (QTP) because of the high altitude and complex terrain. The accuracy of satellite-based gridded precipitation products have been continuously improved recently which is crucial to the study of cryosphere ecology and environment. The goal of this study is to evaluate the accuracy of CHIRPS v2 (Climate Hazards Group Infrared Precipitation with Stations data, version 2) and MSWEP v2 (Multi-source weighted-Ensemble Precipitation, version 2) daily-precipitation products over the QTP during the period 1981-2015. Validation was done using a time series of daily-precipitation data obtained from 104 hydrometeorological stations distributed over the QTP. Error metrics (The correlation coefficient CC, the relative bias BIAS, and root mean square error RMSE) were used for accuracy evaluation and detectability indicators (probability of detection POD, false alarm ratio RFA, and critical success index CSI) were used for the analysis of detection capabilities of rainfall occurrence events. The results indicate that when compared to rain gauge observations, CHIRPS and MSWEP daily-precipitation products represent well the spatial and temporal distribution of the mean daily precipitation over the QTP, while both of them overestimate the daily-precipitation (0.18 mm/d for CHIRPS, 0.56 mm/d for MSWEP). MSWEP performed better than CHIRPS according to CC (MSWEP is 0.44, CHIRPS is 0.23) and RMSE (MSWEP is 4.21 mm, CHIRPS is 5.03 mm) and MSWEP showed better detection capabilities with higher POD (0.65), lower RFA (0.50) and higher CSI (0.39) in the QTP. Both products are less accurate in dry conditions (the north QTP, winter) than in moist conditions (the south QTP, summer). Light precipitation events (0-2 mm/d) are underestimated but heavy precipitation events (2-25 mm/d) are overestimated. CHIRPS and MSWEP have shown great potential to be able to be applied to the precipitation-related study of the QTP. Although the accuracy of MSWEP is higher than that of CHIRPS, the latter has higher spatial resolution (o.o5 degrees) and is more suitable for small-scale studies.
机译:由于高海拔和复杂的地形,在青藏高原(QTP)上,高分辨率,长期,准确的日降水总是很困难,而且很少测量。近年来,基于卫星的网格降水产品的精度一直在不断提高,这对于冰冻圈生态和环境的研究至关重要。这项研究的目的是评估QIR期间QIR上CHIRPS v2(带站数据的气候灾害组红外降水,版本2)和MSWEP v2(多源加权集合降水,版本2)在QTP上的准确性。 1981-2015年。使用从QTP上分布的104个水文气象站获得的每日降水数据的时间序列进行验证。误差度量(相关系数CC,相对偏差BIAS和均方根误差RMSE)用于准确性评估,而可检测性指标(检测POD概率,误报率RFA和关键成功指数CSI)用于分析。降雨发生事件的检测能力。结果表明,与雨量计观测值相比,CHIRPS和MSWEP日降水量产品很好地代表了QTP上的平均日降水量的时空分布,而两者均高估了日降水量(CHIRPS为0.18 mm / d ,对于MSWEP为0.56 mm / d)。根据CC(MSWEP为0.44,CHIRPS为0.23)和RMSE(MSWEP为4.21 mm,CHIRPS为5.03 mm),MSWEP的性能优于CHIRPS,MSWEP表现出更好的检测能力,其中POD较高(0.65),RFA较低(0.50)和更高QTP中的CSI(0.39)。两种产品在干燥条件下(北部QTP,冬季)的准确性均不如在潮湿条件下(南部QTP,夏季)。轻度降水事件(0-2 mm / d)被低估,而重度降水事件(2-25 mm / d)被高估。 CHIRPS和MSWEP已显示出巨大的潜力,可用于QTP的降水相关研究。尽管MSWEP的准确性高于CHIRPS,但后者具有更高的空间分辨率(o.o5度),更适合于小型研究。

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