Titlebook: Ocean Colour: Theory and Applications in a Decade of CZCS Experience; Vittorio Barale,Peter M. Schlittenhardt Book 1993 Springer Science+B

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Underwater Light Field and Primary Production: Application to Remote Sensing,sists of the development of a local algorithm to compute the photosynthetic rate by phytoplankton, and the application of this local result to estimate the integrated primary production at larger scales. Based on the well known relationship between light and photosynthesis, the local model uses spec

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CZCS Data Processing Algorithms,posed algorithm (.) using a water optical model for case 1 waters and allowing a pixel-bypixel evaluation of AE and pigment are discussed. Results of a study of sensitivity loss of CZCS are presented and compared with results of other investigations.

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Ocean Colour and CZCS Applications in and Around Europe,ner (CZCS) experiment, with the development of algorithms and models to handle data calibration, atmospheric correction, pigment value retrieval. Special requirements have been imposed on such developments by the peculiarity of the European basins. The Seas of Europe present an heterogeneous mixture

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Special Features and Applications of CZCS Data in Asian Waters,ely high aerosol concentration and another being the effect of Asian Dust (or KOSA - Yellow Sand Dust). A CZCS image affected by a KOSA event in May, 1981 will be shown. An attempt for a new atmospheric correction scheme tuned for that unique aerosol will also be presented. The paper then reviews an

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Global Oceanic Production and Climate Change,biomass are geographically separated and distinct. Three main regions can be distinguished - the northern hemisphere temperate oceans, the Equatorial divergences and the southern hemisphere temperate waters around 40–50°S. In the three regions the large scale mechanisms which control algal growth an

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Coupling of Ocean Color Data to Physical-Biological Models, are useful for quantitative analyses of ocean color data and satellite-derived phytoplankton fields can be used for initialization and verification of physical-biological models. Also assimilation of phytoplankton fields, derived from ocean color measurements, into physical-biological models repres

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Ocean Colour in Relation to Biological Patterns and Processes in a Biogeographical Province,ent scales. At the mesoscale (hundreds of kilometers, months to years), the major biological patterns, and associated processes, in summer are the following. A meandering jet, entraining high pigment filaments that occur on the inshore side of the jet, and interacting strongly with anticyclonic, low

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Seasonal and Meridional Variability of the Remotely Sensed Fraction of Euphotic Zone Chlorophyll Pryll (EZC), which are caused by changes in the vertical chlorophyll distribution related to the succession of growth phases during the phytoplankton seasonal cycle in mid-latitudes. In order to assess how accurately satellite color signals represent the total euphotic zone phytoplankton biomass, the