The retrieval of aerosol and cloud properties such as their optical thickness and/or layer/top height requires the selection of a model that describes their microphysical properties. We demonstrate that, if there is not enough information for an appropriate microphysical model selection, the solution’s accuracy can be improved if the model uncertainty is taken into account and appropriately quantified. For this purpose, we design a retrieval algorithm accounting for the uncertainty in model selection. The algorithm is based on (i) the computation of each model solution using the iteratively regularized Gauss–Newton method, (ii) the linearization of the forward model around the solution, and (iii) the maximum marginal likelihood estimation a...
Stratospheric aerosol particles under non-volcanic conditions are typically smaller than 0.1 μ m. Du...
Due to similarities in their radiometric signature, it is not possible to retrieve aerosol and cloud...
Stratospheric aerosol particles under non-volcanic conditions are typically smaller than 0.1 μm. Due...
Satellite instruments are nowadays successfully utilised for measuring atmospheric aerosol in many a...
Satellite instruments are nowadays successfully utilised for measuring atmospheric aerosol in many a...
To retrieve aerosol properties from satellite measurements, micro-physical aerosol models have to be...
To retrieve aerosol properties from satellite measurements, micro-physical aerosol models have to be...
We have developed a new algorithm for the retrieval of aerosol and gases from SAGE It1 solar transmi...
We discuss uncertainty quantification for aerosol-type selection in satellite-based atmospheric aer...
Atmospheric aerosols play a central role in the Earth's radiative budget. Together with various gree...
Atmospheric aerosols play a central role in the Earth's radiative budget. Together with various gree...
The Multi-sensor Cloud Retrieval Simulator (MCRS) produces a simulated radiance product from any hig...
Aerosols are the source of the largest uncertainties in our climate models, blurring our outlook of ...
Aerosols are the source of the largest uncertainties in our climate models, blurring our outlook of ...
Due to similarities in their radiometric signature, it is not possible to retrieve aerosol and cloud...
Stratospheric aerosol particles under non-volcanic conditions are typically smaller than 0.1 μ m. Du...
Due to similarities in their radiometric signature, it is not possible to retrieve aerosol and cloud...
Stratospheric aerosol particles under non-volcanic conditions are typically smaller than 0.1 μm. Due...
Satellite instruments are nowadays successfully utilised for measuring atmospheric aerosol in many a...
Satellite instruments are nowadays successfully utilised for measuring atmospheric aerosol in many a...
To retrieve aerosol properties from satellite measurements, micro-physical aerosol models have to be...
To retrieve aerosol properties from satellite measurements, micro-physical aerosol models have to be...
We have developed a new algorithm for the retrieval of aerosol and gases from SAGE It1 solar transmi...
We discuss uncertainty quantification for aerosol-type selection in satellite-based atmospheric aer...
Atmospheric aerosols play a central role in the Earth's radiative budget. Together with various gree...
Atmospheric aerosols play a central role in the Earth's radiative budget. Together with various gree...
The Multi-sensor Cloud Retrieval Simulator (MCRS) produces a simulated radiance product from any hig...
Aerosols are the source of the largest uncertainties in our climate models, blurring our outlook of ...
Aerosols are the source of the largest uncertainties in our climate models, blurring our outlook of ...
Due to similarities in their radiometric signature, it is not possible to retrieve aerosol and cloud...
Stratospheric aerosol particles under non-volcanic conditions are typically smaller than 0.1 μ m. Du...
Due to similarities in their radiometric signature, it is not possible to retrieve aerosol and cloud...
Stratospheric aerosol particles under non-volcanic conditions are typically smaller than 0.1 μm. Due...