2015
DOI: 10.1016/j.rser.2015.01.065
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Validation of direct normal irradiance predictions under arid conditions: A review of radiative models and their turbidity-dependent performance

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Cited by 84 publications
(37 citation statements)
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“…The present findings clearly suggest that the modeling of radiative aerosol effects is the most likely cause of discrepancy between modeled predictions, thus confirming previous site-specific evaluations, e.g. [5,7,9].…”
Section: Resultssupporting
confidence: 89%
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“…The present findings clearly suggest that the modeling of radiative aerosol effects is the most likely cause of discrepancy between modeled predictions, thus confirming previous site-specific evaluations, e.g. [5,7,9].…”
Section: Resultssupporting
confidence: 89%
“…Aerosol optical depth at 500, 469, 670 and 865 nm are retrieved from MACC. The Ångström turbidity coefficient and exponent are calculated from a log-log fit of these spectral AODs to the Ångström formula (see [5] for details). The aerosol optical depths at 550 and 700 nm are derived using the Ångström formula with the Ångström exponent and AOD at 500 and 670 nm, respectively.…”
Section: Data and Clear-sky Solar Radiation Modelsmentioning
confidence: 99%
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“…However, most locations lack long-term accurate radiation, cloudiness, and/or satellite data for many climate stations, which are needed in order to identify and estimate atmospheric attenuation. For example, models such as r.sun [16,17], Solei-32 [17,18] and, ESRA [5,6,8] calculate the overcast radiation from clear sky values and a clear-sky index called Linke (Table 1, [23,24]). The Linke must be derived from one of the three methods: (1) from the ratio between measured global radiation and computed values of clear sky global radiation, (2) from other climatologic data such as cloudiness [23], or (3) directly from shortwave surface irradiance measured by satellites [24].…”
Section: Introductionmentioning
confidence: 99%