Add to ORKGThe attenuating properties of the atmosphere are presented in a form that permits the calculation of direct, diffuse and global spectral solar irradiance at ground level, using the extraterrestrial irradiance values of Thekaekara. Input data describing the state of the atmosphere are obtained from standard meteorological information or from tabulated average values. Clear sky diffuse spectral irradiance on a horizontal surface is estimated from the direct beam by means of an empirical simplification. Examples of the agreement between calculated and measured values are shown
Spectral distributions of solar radiation were measured over the wavelength range 300 to 800 nm in N...
The estimation of the irradiance of sloping surfaces from standard meteorological measurements requi...
A mathematical model has been developed for predicting the spectral distribution of solar radiation ...
The attenuating properties of the atmosphere are presented in a form that permits the calculation of...
A simple empirical model to calculate solar spectral diffuse and global irradiance under cloudless s...
A simple empirical model to calculate solar spectral diffuse and global irradiance under cloudless s...
The downwelling solar irradiance received at ground level has many effects on many aspects, from cli...
Available quantitative data on solar total and spectral irradiance are examined in the context of ut...
Measurements of cloudless direct, global, and diffuse solar radiations, taken over a one year period...
A technique was developed to produce maps of the distribution of diffuse solar radiation over the sk...
Solar radiation is modified in its way downwards by the content of the atmosphere. Quantifying the i...
International audienceThe k-distribution method and the correlated-k approximation of Kato et al. (1...
Atmosphere scatters and absorbs incident solar radiation modifying its spectral content and decreasi...
Solar radiation is modified in its way downwards by the content of the atmosphere. Quantifying the ...
Physical and empirical models for calculation of insolation on a horizontal surface are described. C...
Spectral distributions of solar radiation were measured over the wavelength range 300 to 800 nm in N...
The estimation of the irradiance of sloping surfaces from standard meteorological measurements requi...
A mathematical model has been developed for predicting the spectral distribution of solar radiation ...
The attenuating properties of the atmosphere are presented in a form that permits the calculation of...
A simple empirical model to calculate solar spectral diffuse and global irradiance under cloudless s...
A simple empirical model to calculate solar spectral diffuse and global irradiance under cloudless s...
The downwelling solar irradiance received at ground level has many effects on many aspects, from cli...
Available quantitative data on solar total and spectral irradiance are examined in the context of ut...
Measurements of cloudless direct, global, and diffuse solar radiations, taken over a one year period...
A technique was developed to produce maps of the distribution of diffuse solar radiation over the sk...
Solar radiation is modified in its way downwards by the content of the atmosphere. Quantifying the i...
International audienceThe k-distribution method and the correlated-k approximation of Kato et al. (1...
Atmosphere scatters and absorbs incident solar radiation modifying its spectral content and decreasi...
Solar radiation is modified in its way downwards by the content of the atmosphere. Quantifying the ...
Physical and empirical models for calculation of insolation on a horizontal surface are described. C...
Spectral distributions of solar radiation were measured over the wavelength range 300 to 800 nm in N...
The estimation of the irradiance of sloping surfaces from standard meteorological measurements requi...
A mathematical model has been developed for predicting the spectral distribution of solar radiation ...