2022
DOI: 10.1016/j.jhydrol.2022.127430
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Rainfall estimation from surface soil moisture using SM2RAIN in cold mountainous areas

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Cited by 12 publications
(3 citation statements)
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“…The annual average temperature at the AGS is from −3.1 to 3.6 • C, and the annual average precipitation, most of which occurs from June to September, is about 300-600 mm [2,19,47]. Both observation sites have been used by a number of studies as good representatives of the study area [61][62][63][64]. The measurement of the CRNS observation reliability at the two observation sites has also been adequately verified by previous studies [48,64].…”
Section: Study Areasmentioning
confidence: 55%
“…The annual average temperature at the AGS is from −3.1 to 3.6 • C, and the annual average precipitation, most of which occurs from June to September, is about 300-600 mm [2,19,47]. Both observation sites have been used by a number of studies as good representatives of the study area [61][62][63][64]. The measurement of the CRNS observation reliability at the two observation sites has also been adequately verified by previous studies [48,64].…”
Section: Study Areasmentioning
confidence: 55%
“…The bottom-up approach has been applied at a global scale 23 , 24 and a local scale in Asia 25 28 , Australia 29 , 30 , Europe 31 , 32 , Africa 33 , 34 , and America 35 , 36 . More than 150 papers have been published in peer-reviewed journals related to SM2RAIN rainfall products, which have highlighted the high potential of this approach over different parts of the globe and also the effectiveness of them in many applications including flood prediction 37 , water resources management 38 , and prediction of landslide 39 , soil erosion 33 , and crop yield 40 .…”
Section: Background and Summarymentioning
confidence: 99%
“…Once ET is calculated for a specific vegetation condition (ET0), the "crop coefficient" (Kc) can be applied to convert it for other vegetation types (Allen et al, 1998). This approach has been proven to be more cost-effective to estimate ET0 by utilizing other meteorological variables, although direct measuring of ET can be applied using lysimeters or the turbulent vortex covariance method (Lai et al, 2023). ETP and ET0 can be applied to different applications, where ETP is considered more general and suitable for larger areas, while ET0 is more specific and, therefore, particularly useful for project planning in small areas (Xiang et al, 2022).…”
Section: Introductionmentioning
confidence: 99%