2018
DOI: 10.3390/atmos9040117
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Estimating Hourly Beam and Diffuse Solar Radiation in an Alpine Valley: A Critical Assessment of Decomposition Models

Abstract: Accurate solar radiation estimates in Alpine areas represent a challenging task, because of the strong variability arising from orographic effects and mountain weather phenomena. These factors, together with the scarcity of observations in elevated areas, often cause large modelling uncertainties. In the present paper, estimates of hourly mean diffuse fraction values from global radiation data, provided by a number (13) of decomposition models (chosen among the most widely tested in the literature), are evalua… Show more

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Cited by 17 publications
(7 citation statements)
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References 77 publications
(78 reference statements)
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“…Water 2018, 10, x FOR PEER REVIEW 13 of 15 metamorphism process is controlled by solar radiation. Over mountainous areas, the distribution of solar radiation is affected by topography, including elevation, slope, and aspect [39], which affect the snow accumulation and snowmelt owing to the different radiation and energy balances. Therefore, snow distribution is controlled by the terrain in an alpine watershed [40].…”
Section: Discussionmentioning
confidence: 99%
“…Water 2018, 10, x FOR PEER REVIEW 13 of 15 metamorphism process is controlled by solar radiation. Over mountainous areas, the distribution of solar radiation is affected by topography, including elevation, slope, and aspect [39], which affect the snow accumulation and snowmelt owing to the different radiation and energy balances. Therefore, snow distribution is controlled by the terrain in an alpine watershed [40].…”
Section: Discussionmentioning
confidence: 99%
“…Among the numerous decomposition models proposed in the literature (Bertrand et al, 2015), the model of Skartveit et al (1998) is used. This model is among the most widespread and has recently been found to be one of the most efficient in a comparison with 13 other models for a highly rugged area near Bolzano (northern Italy) (Laiti et al, 2018). The model is based on three main input predictors: the solar zenith angle, the clearness index and a temporal variability index (hourly in the original model and semi-hourly in ERAD).…”
Section: Half-hourly Data Processingmentioning
confidence: 99%
“…Individual components of the radiation balance are typically made with high-quality, carefully calibrated pyranometers and pyrgeometers. The radiation balance in mountainous regions is complicated by a range of factors including heterogeneity of surface radiative properties, roughness elements covering a range of scales, non-uniform aerosol distributions, different vegetation covers, as well as reduced and complex sky view factors and extended shadowing [67]. These different factors may lead to surface radiation balances that differ greatly from flat homogeneous terrain [63].…”
Section: Radiationmentioning
confidence: 99%