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Titlebook: Remote Sensing of Atmosphere and Ocean from Space: Models, Instruments and Techniques; Frank S. Marzano,Guido Visconti Book 2002 Springer

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Sea Surface Characterization by Combined Datae the sub-basin and mesoscale dynamic features of the Mediterranean circulation. The resulting picture of the surface circulation obtained satellite observations are compared with concurrent . and modelled data.
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Atmospheric Backscatter and Lidarssing systems are very efficient at detecting atmospheric minor constituents with high spatial and temporal resolution. In particular, we shall address lidar observations of atmospheric aerosols, one of the major unknowns in the Earth’s climate system. The fundamental tools for a quantitative retriev
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Precipitation Modeling for Inversion Purposesiation scattering and emission in atmosphere, clouds, and interaction with surfaces. This involves the evaluation of the significance of individual effects with respect to the observed signals. In case of microwave radiation, these effects are the three-dimensional distribution of temperature, humid
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Bayesian Techniques in Remote Sensingr, Bayesian criterion to test hypothesis is described to solve a data classification problem. Bayesian estimation of unknown parameters is presented as a method to invert direct electromagnetic models. The use of contextual information when dealing with images is also shortly described.
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Microwave Limb Sounding as a technique for the observation of tropospheric trace gas species. The article introduces the most important past and future instruments of this type, as well as some basics of the technique. A comprehensive list of references will make it possible for the interested reader to obtain more detail
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Retrieval of Integrated Water Vapour and Cloud Liquid Water Contentsur content was performed first with the ESMR (Electrically Scanning Microwave Radiometer) flown on the Nimbus-5 satellite, then operational products from the SMMR (Scanning Multichannel Microwave Radiometer) onboard SEASAT and Nimbus-7 were routinely delivered (Wilheit and Chang, 1980, Prabhakara et
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