2021
DOI: 10.1016/j.atmosres.2021.105459
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Evaluation of fine resolution gridded rainfall datasets over a dense network of rain gauges in Niger

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Cited by 14 publications
(7 citation statements)
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“…On the daily scale, all products generally show a low correlation with observed precipitation. In the YZR, the CC values of daily precipitation range from 0.30 to 0.39, which is lower than the values of the same products in other basins, such as Huifa River [27], Blue Nile [52], Huaihe River [13], etc. It can be further seen from the statistical and categorical metrics that the accuracy of the satellite precipitation products has a strong dependence on rainfall intensity [24].…”
Section: Results Of Grid-point Validationmentioning
confidence: 70%
“…On the daily scale, all products generally show a low correlation with observed precipitation. In the YZR, the CC values of daily precipitation range from 0.30 to 0.39, which is lower than the values of the same products in other basins, such as Huifa River [27], Blue Nile [52], Huaihe River [13], etc. It can be further seen from the statistical and categorical metrics that the accuracy of the satellite precipitation products has a strong dependence on rainfall intensity [24].…”
Section: Results Of Grid-point Validationmentioning
confidence: 70%
“…The traditional method for obtaining precipitation data is to install a network of rain gauge stations with a specific spatial density. Although accurate precipitation can be obtained at each station, the uneven distribution of rain gauge stations and the spatial discontinuity of precipitation data have obvious limitations [6,7]. Remote-sensing-based methods using radars or satellites have been increasingly applied to estimate precipitation and spatial distribution.…”
Section: Introductionmentioning
confidence: 99%
“…Selection of the most suitable GPD based on their capability to capture the different characteristics of observed rainfall, such as mean, variability, probability distribution, extremes, seasonal fluctuation, and geographical distribution, is always difficult (Gampe et al ., 2019; Musie et al ., 2019). Various techniques have been used in literature for selecting suitable GPD (Ahmed et al ., 2017; Faiz et al ., 2018; Salman et al ., 2019; Yao et al ., 2020; Abdourahamane, 2021; Wang et al ., 2021). Most of the studies used different combinations of conventional statistics, such as coefficient of determination ( R 2 ), mean error, or mean bias to assess different characteristics of GPDs (Chen et al ., 2017; Faiz et al ., 2018; Hu et al ., 2018; Yeggina et al ., 2019; Salman et al ., 2019; Giles et al ., 2020; Abdourahamane, 2021; Dahri et al ., 2021; Merino et al ., 2021).…”
Section: Introductionmentioning
confidence: 99%
“…Various techniques have been used in literature for selecting suitable GPD (Ahmed et al ., 2017; Faiz et al ., 2018; Salman et al ., 2019; Yao et al ., 2020; Abdourahamane, 2021; Wang et al ., 2021). Most of the studies used different combinations of conventional statistics, such as coefficient of determination ( R 2 ), mean error, or mean bias to assess different characteristics of GPDs (Chen et al ., 2017; Faiz et al ., 2018; Hu et al ., 2018; Yeggina et al ., 2019; Salman et al ., 2019; Giles et al ., 2020; Abdourahamane, 2021; Dahri et al ., 2021; Merino et al ., 2021). Besides, the GPDs have been evaluated based on their ability to simulated different hydrological events such as surface runoff (Try et al ., 2020), floods (Nashwan et al ., 2019), droughts (Centella‐Artola et al ., 2020) and crop yield (Lashkari et al ., 2018).…”
Section: Introductionmentioning
confidence: 99%