It is well known that including the delta-scaling in the radiative transfer calculation improves the accuracy of radiative transfer in a cloud layer. An improved scheme is proposed to handle the delta-scaling in the radiative transfer calculation. The improved scheme is able to calculate irradiance of a vertical inhomogeneous cloud layer. The inherent optical properties (IOPs) in a cloud layer vary with height. Linear functions are used to represent the variation of IOPs. Compared to the exponential expression, the linear functions simplified the representation of IOPs. A perturbation method based on Eddington approximation is applied to solve the radiative transfer equation. The accuracy of the proposed scheme is evaluated by comparing ref...
To relate the error associated with 1D radiative calculations to the geometrical scales of cloud org...
Top of the atmosphere synthetic spectral radiances are computed for widespread atmospheric condition...
International audienceThe multiresolution radiative transfer equations of Part I of this paper are s...
A multi-layer solar radiative transfer (RT) scheme is proposed to deal with the vertical variation o...
Analytical approaches have been developed for one-dimensional monochromatic delta-Eddington radiativ...
A new scheme based on perturbation method is presented to solve the problem of solar/infrared radiat...
The DIScrete Ordinate Radiative Transfer (DISORT) and the delta-Eddington models were used to evalua...
A multilevel spectral radiative transfer model is used to develop simple but accurate parameterizati...
The radiative transfer perturbation theory (RTPT), which has already been introduced in atmospheric ...
The 4DCLOUDS project was established to gain a more accurate understanding of the role clouds play i...
The role of horizontal inhomogeneity in radiative transfer through cloud fields is investigated with...
Abstract. The authors introduce a radiative transfer model CLOUD for reflection, transmission, and a...
This work contributes to the research of fast calculations of the surface solar irradiance (SSI) I a...
[1] Radiative transfer schemes in large-scale models tightly couple assumptions about cloud structur...
Top of the atmosphere synthetic spectral radiances are computed for widespread atmospheric condition...
To relate the error associated with 1D radiative calculations to the geometrical scales of cloud org...
Top of the atmosphere synthetic spectral radiances are computed for widespread atmospheric condition...
International audienceThe multiresolution radiative transfer equations of Part I of this paper are s...
A multi-layer solar radiative transfer (RT) scheme is proposed to deal with the vertical variation o...
Analytical approaches have been developed for one-dimensional monochromatic delta-Eddington radiativ...
A new scheme based on perturbation method is presented to solve the problem of solar/infrared radiat...
The DIScrete Ordinate Radiative Transfer (DISORT) and the delta-Eddington models were used to evalua...
A multilevel spectral radiative transfer model is used to develop simple but accurate parameterizati...
The radiative transfer perturbation theory (RTPT), which has already been introduced in atmospheric ...
The 4DCLOUDS project was established to gain a more accurate understanding of the role clouds play i...
The role of horizontal inhomogeneity in radiative transfer through cloud fields is investigated with...
Abstract. The authors introduce a radiative transfer model CLOUD for reflection, transmission, and a...
This work contributes to the research of fast calculations of the surface solar irradiance (SSI) I a...
[1] Radiative transfer schemes in large-scale models tightly couple assumptions about cloud structur...
Top of the atmosphere synthetic spectral radiances are computed for widespread atmospheric condition...
To relate the error associated with 1D radiative calculations to the geometrical scales of cloud org...
Top of the atmosphere synthetic spectral radiances are computed for widespread atmospheric condition...
International audienceThe multiresolution radiative transfer equations of Part I of this paper are s...