The Community Cloud retrieval for CLimate (CC4CL). Part II: The optimal estimation approach
Atmospheric Measurement Techniques Discussions European Geosciences Union (2017)
Abstract:
The Community Cloud retrieval for Climate (CC4CL) is a cloud property retrieval system for satellite-based multispectral imagers and is an important component of the Cloud Climate Change Initiative (Cloud_cci) project. In this paper we discuss the optimal estimation retrieval of cloud optical thickness, effective radius and cloud top pressure based on the Optimal Retrieval of Aerosol and Cloud (ORAC) algorithm. Key to this method is the forward model which, includes the 5 clear-sky model, the liquid water and ice cloud models, the surface model including a bidirectional reflectance distribution function (BRDF), the “fast” radiative transfer solution (which includes a multiple scattering treatment) All of these components and their assumptions and limitations will be discussed in detail. The forward model provides the accuracy appropriate for our retrieval method. The errors are comparable to the instrument noise for cloud optical thicknesses greater than 10. At optical thicknesses less than 10 modelling errors become more significant. The retrieval method is then presented describing 10 optimal estimation in general, the non-linear inversion method employed, measurement and a priori inputs, the propagation of input uncertainties and the calculation of subsidiary quantities that are derived from the retrieval results. An evaluation of the retrieval was performed using measurements simulated with noise levels appropriate for the MODIS instrument. Results show errors less than 10% for cloud optical thicknesses greater than 10. Results for clouds of optical thicknesses less than 10 have errors ranging up to 20%.The origin of methane and biomolecules from a CO2 cycle on terrestrial planets
Nature Astronomy Springer Science and Business Media LLC 1:10 (2017) 721-726
Mass extinction spectra and size distribution measurements of quartz and amorphous silica aerosol at 0.33-19 mu m compared to modelled extinction using Mie, CDE, and T-matrix theories
JOURNAL OF QUANTITATIVE SPECTROSCOPY & RADIATIVE TRANSFER 199 (2017) 52-65
Retrieval of volcanic SO2 from HIRS/2 using optimal estimation
ATMOSPHERIC MEASUREMENT TECHNIQUES 10:7 (2017) 2687-2702
Retrieval of volcanic SO2 from HIRS/2 using optimal estimation
Atmospheric Measurement Techniques Discussions (2017) 1-30