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      An evaluation of marine regions relevant for ocean color system vicarious calibration

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          Abstract

          System Vicarious Calibration (SVC) is the fundamental process commonly implemented to meet uncertainty requirements in satellite ocean color data. It is performed by applying gain factors, g-factors, to the pre-launch calibration coefficients of the space sensor already corrected for sensitivity decay with time. Mission specific g-factors are determined from top-of-the-atmosphere data computed by propagating highly accurate in situ values of the water-leaving radiance, L w, to the satellite sensor. Values of L w from marine regions characterized by oligotrophic/mesotrophic waters and maritime aerosols, high environmental stability and spatial homogeneity, low cloudiness and absence of any source of land contamination, are essential to determine g-factors applicable to the creation of Climate Data Records (CDRs) from multiple ocean color missions. Accounting for the location of existing and potential new SVC fixed sites, marine regions satisfying SVC requirements for the generation of CDRs have been identified through the analysis of satellite data from recent ocean color missions.

          Highlights

          • System Vicarious Calibration (SVC) for ocean color missions

          • Climatology of marine and atmospheric optical properties of regions relevant for SVC

          • Recommendations for new SVC regions

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          Most cited references61

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          Aerosols, climate, and the hydrological cycle.

          Human activities are releasing tiny particles (aerosols) into the atmosphere. These human-made aerosols enhance scattering and absorption of solar radiation. They also produce brighter clouds that are less efficient at releasing precipitation. These in turn lead to large reductions in the amount of solar irradiance reaching Earth's surface, a corresponding increase in solar heating of the atmosphere, changes in the atmospheric temperature structure, suppression of rainfall, and less efficient removal of pollutants. These aerosol effects can lead to a weaker hydrological cycle, which connects directly to availability and quality of fresh water, a major environmental issue of the 21st century.
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            Global air pollution crossroads over the Mediterranean.

            The Mediterranean Intensive Oxidant Study, performed in the summer of 2001, uncovered air pollution layers from the surface to an altitude of 15 kilometers. In the boundary layer, air pollution standards are exceeded throughout the region, caused by West and East European pollution from the north. Aerosol particles also reduce solar radiation penetration to the surface, which can suppress precipitation. In the middle troposphere, Asian and to a lesser extent North American pollution is transported from the west. Additional Asian pollution from the east, transported from the monsoon in the upper troposphere, crosses the Mediterranean tropopause, which pollutes the lower stratosphere at middle latitudes.
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              Merged satellite ocean color data products using a bio-optical model: Characteristics, benefits and issues

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                Author and article information

                Contributors
                Journal
                Remote Sens Environ
                Remote Sens Environ
                Remote Sensing of Environment
                American Elsevier Pub. Co
                0034-4257
                1879-0704
                01 March 2017
                01 March 2017
                : 190
                : 122-136
                Affiliations
                European Commission, Joint Research Centre, Ispra, Italy
                Author notes
                Article
                S0034-4257(16)30467-9
                10.1016/j.rse.2016.11.020
                5312659
                1fd786f6-30fd-494e-9f3f-fb811379bb3a
                © 2016 The Authors

                This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).

                History
                : 22 May 2016
                : 17 November 2016
                : 27 November 2016
                Categories
                Article

                ocean color,system vicarious calibration
                ocean color, system vicarious calibration

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