2019
DOI: 10.1016/j.jksus.2017.06.002
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Estimation of atmospheric turbidity over Adrar city in Algeria

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Cited by 9 publications
(5 citation statements)
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“…With regard to the semi-empirical approach, the complexity of the clear-sky irradiance model, which is caused by rapid changes in aerosols, water vapor, and other molecules, is relatively reduced. The atmospheric variables can instead be simplified into a single turbidity variable of T L [35][36][37]. In this study, well-known clear-sky irradiance models (Table 3) were selected to examine GHI c .…”
Section: Clear-sky Irradiance Formulamentioning
confidence: 99%
“…With regard to the semi-empirical approach, the complexity of the clear-sky irradiance model, which is caused by rapid changes in aerosols, water vapor, and other molecules, is relatively reduced. The atmospheric variables can instead be simplified into a single turbidity variable of T L [35][36][37]. In this study, well-known clear-sky irradiance models (Table 3) were selected to examine GHI c .…”
Section: Clear-sky Irradiance Formulamentioning
confidence: 99%
“…We can explain it by winds of the south sectors (Sirocco) during the summer season that characterize the Sahara of North Africa. This kind of winds brings particles of dust and sand with them, which increases the Angström coefficient [1,19,20,32,41].…”
Section: Resultsmentioning
confidence: 99%
“…We note that there is a temporal extremum of β (middle plot in Figure 8) while there is an extremum in both humidity and temperature at the same time (bottom plot in Figure 9). These seasonal variations are most likely related to the African monsoon [1,20,32,41,42]. ± 0.04 0.12 ± 0.05 0.15 ± 0.04 0.11 ± 0.03 September 0.14 ± 0.05 0.13 ± 0.04 0.11 ± 0.06 0.11 ± 0.06 0.12 ± 0.03 0.14 ± 0.04 October 0.12 ± 0.05 0.14 ± 0.04 0.09 ± 0.04 0.09 ± 0.04 0.14 ± 0.04 0.16 ± 0.08 November 0.12 ± 0.06 0.13 ± 0.05 0.02 ± 0.03 0.02 ± 0.02 0.14 ± 0.05 0.11 ± 0.04 December 0.11 ± 0.03 0.11 ± 0.05 0.03 ± 0.05 0.03 ± 0.03 0.12 ± 0.06 0.11 ± 0.05 Finally, we compared the Angström coefficient obtained with ESRA 2 model with the frequency of occurrence of aerosols over Tamanrasset observed from space.…”
Section: Resultsmentioning
confidence: 99%
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“…The respective MBE of DNI and T L are 0.91% and 1.31%, which shows the accuracy of the model despite its simplicity. In Northern Africa, Marif et al[88] (Algeria, 31 months) studied the turbidity and developed a CSI model, they confirmed that T L and β are highly affected by wind speed, ambient temperature, and humidity. Aerosols' loads were high in summer and low in winter.…”
mentioning
confidence: 91%