2020
DOI: 10.1007/s41748-020-00185-3
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Evaluation of TRMM 3B42V7 and CHIRPS Satellite Precipitation Products as an Input for Hydrological Model over Eastern Nile Basin

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Cited by 40 publications
(13 citation statements)
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“…8.2a. (Kojiri et al 1998;Abdelmoneim et al 2020) Each mesh cell includes details such as surface runoff, land use, slope direction, and a channel's absence/presence (Saber 2010). Layer A represents the surface layer, while layers B to D represent the subsurface layers, as denoted in Fig.…”
Section: Gpcp-1dd Productmentioning
confidence: 99%
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“…8.2a. (Kojiri et al 1998;Abdelmoneim et al 2020) Each mesh cell includes details such as surface runoff, land use, slope direction, and a channel's absence/presence (Saber 2010). Layer A represents the surface layer, while layers B to D represent the subsurface layers, as denoted in Fig.…”
Section: Gpcp-1dd Productmentioning
confidence: 99%
“…The model was confined to environments characterized by moist circumstances until the model was adjusted for simulations of flash flood events in arid wadis(Abdel-Fattah et al 2015;Saber et al 2013) and semiarid basins (Abdel-Fattah 2017; Saber and Yilmaz 2016). The model has also been successfully used in numerous hydrological studies under different climatic conditions (e.g., Abd-ElMoneim et al 2017;Saber and Yilmaz 2018;Abdelmoneim et al 2020). In this study, Hydro-BEAM is used to evaluate the simulated streamflow rates over the BNB based on six PESPs.…”
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confidence: 99%
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“…The emergence of hyperspectral remote sensing technology is undoubtedly a breakthrough in the field of remote sensing [1][2][3]. Hyperspectral sensors with dozens or even hundreds of spectral bands may effectively capture abundant spectral and spatial information on the Earth's surface.…”
Section: Introductionmentioning
confidence: 99%
“…The data are relatively accurate and are collected at relatively high frequencies [9]. However, it is more difficult to obtain representative and long-term precipitation data over complex terrain because of the inhomogeneous and sparse distribution of land gauges and the high costs to build new gauges [10][11][12]. By contrast, passive microwave observations from satellites take into account the interactions between the microwave radiation and the hydrometeors inside clouds and rain, allowing precipitation to be measured globally, extending the dataset collected by land stations.…”
Section: Introductionmentioning
confidence: 99%