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Sea-viewing wide field-of-view sensor

SCOR SeaWiFS Scientific Committee on Ocean Research Sea-viewing Wide Field-of-View Sensor... [Pg.138]

SeaWiFS Sea-viewing wide field-of-view sensor... [Pg.195]

Table 3 Algorithms used to calculate chlorophyll a (C) from remote sensing reflectance. R is determined as the maximum of the values shown. Sensor algorithms are for Sea-viewing Wide Field of view Sensor (SeaWiFS), Ocean Color and Temperature Scanner (OCXS), Moderate Resolution Imaging Spectroradiometer (MODIS), Coastal Zone Color Scanner (CZCS), and Medium Resolution Imaging Spectrometer (MERIS). Table 3 Algorithms used to calculate chlorophyll a (C) from remote sensing reflectance. R is determined as the maximum of the values shown. Sensor algorithms are for Sea-viewing Wide Field of view Sensor (SeaWiFS), Ocean Color and Temperature Scanner (OCXS), Moderate Resolution Imaging Spectroradiometer (MODIS), Coastal Zone Color Scanner (CZCS), and Medium Resolution Imaging Spectrometer (MERIS).
Advanced Very High Resolution Radiometer National Aeronautics and Space Administration National Oceanic and Atmospheric Administration Sea-viewing Wide Field-of-view Sensor Sea-Surface Temperature... [Pg.122]

Fig. 6.2 Monthly climatologies of remotely sensed surface chlorophyll a (a-c) and SST (d-f) for February (a, d), May (b, e) and August (c, f). Chlorophyll and SST climatologies were created by Jerry Wiggert (University of Maryland, College Park) and Bob Evans (RSMAS, University of Miami) using the SeaWiFS (Sea-viewing Wide Field-of-view Sensor) and MODIS (Moderate-resolution Imaging Spectroradiometer) data, respectively. Note that some features of circulation (e.g. the great whirl) can be readily identified in both sets of data (see Color Plate 2). Fig. 6.2 Monthly climatologies of remotely sensed surface chlorophyll a (a-c) and SST (d-f) for February (a, d), May (b, e) and August (c, f). Chlorophyll and SST climatologies were created by Jerry Wiggert (University of Maryland, College Park) and Bob Evans (RSMAS, University of Miami) using the SeaWiFS (Sea-viewing Wide Field-of-view Sensor) and MODIS (Moderate-resolution Imaging Spectroradiometer) data, respectively. Note that some features of circulation (e.g. the great whirl) can be readily identified in both sets of data (see Color Plate 2).
Figure 5 Sea-Viewing Wide Field-of-View Sensor (SeaWiFS) satellite image of an iron-induced phytoplankton bloom in the Southern Ocean. The bloom is apparent as a chlorophyll maximum near the center of the image (66°S, 172°E) large, contiguous white areas represent cloud cover. The image was captured on day 20 of the SOFeX South patch experiment. Coordinates are degrees South and East. Courtesy of the NASA SeaWiFS Project and the Goddard Earth Sciences Data and Information Services Center/Distrihuted Active Archive Center. Figure 5 Sea-Viewing Wide Field-of-View Sensor (SeaWiFS) satellite image of an iron-induced phytoplankton bloom in the Southern Ocean. The bloom is apparent as a chlorophyll maximum near the center of the image (66°S, 172°E) large, contiguous white areas represent cloud cover. The image was captured on day 20 of the SOFeX South patch experiment. Coordinates are degrees South and East. Courtesy of the NASA SeaWiFS Project and the Goddard Earth Sciences Data and Information Services Center/Distrihuted Active Archive Center.
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