1980
DOI: 10.2172/5626683
|View full text |Cite
|
Sign up to set email alerts
|

Direct insolation models

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
30
0

Year Published

2007
2007
2019
2019

Publication Types

Select...
6
4

Relationship

0
10

Authors

Journals

citations
Cited by 70 publications
(30 citation statements)
references
References 10 publications
0
30
0
Order By: Relevance
“…(13) The direct normal total (spectrally integrated) solar irradiance as a function of the air mass (AM) and atmospheric conditions that include the effects of elevation, can be calculated using the Parameterization Model C developed by Iqbal, given in Eq. (19) [78][79][80].…”
Section: Solar Irradiance Conditionsmentioning
confidence: 99%
“…(13) The direct normal total (spectrally integrated) solar irradiance as a function of the air mass (AM) and atmospheric conditions that include the effects of elevation, can be calculated using the Parameterization Model C developed by Iqbal, given in Eq. (19) [78][79][80].…”
Section: Solar Irradiance Conditionsmentioning
confidence: 99%
“…The description can be found in Bird (1980). The model requires 3 input parameters: the water vapor column (in cm), the broadband aerosol optical depth (at 700 nm or calculated from the spectral attenuation at 2 wavelengths commonly used by meteorological networks: 380 and 500 nm), and the total ozone column considered here as constant and equal to 340 Dobson units.…”
Section: Bird Modelmentioning
confidence: 99%
“…When not known, and this is often the case, it can be evaluated from the spectral aerosol optical depth: 700 , this equivalence is only slightly influenced by the air mass, -or with the help of the empirical Bird and Huldstrom (1980) approximation based on the attenuation at two wavelengths commonly used by meteorological networks: D a = 0.2758 Ã aod 380 + 0.35 Ã aod 500 , where aod k is the aerosol optical depth at the considered wave length k. The extension of the Linke turbidity coefficient to other values of the air mass was published by Ineichen and Perez (2002). In order to extend its validity to higher atmospheric water vapor content and to introduce altitude dependence, a new formulation is proposed.…”
Section: Conversion Functionmentioning
confidence: 99%