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Distribution of sea surface temperature observed on April 25, 1997 by the infrared band of Ocean Colour and Temperature Sensor (OCTS IR) onboard The Japanese ADEOS satellite
NASDA
Phytoplankton (chlorophyll-a) concentration in Japanese waters observed on April 25, 1997 by visible near infrared band of the Ocean Colour and Temperature Scanner (OCTS VNIR) onboard the Japanese Satellite ADEOS.
NASDA
VIIRS-SNPP four month composite images (2014 October through 2015 January) of Chlorophyll a concentration (top) and the spectral attenuation coefficient at 490 nm (bottom) processed using NOAA-MSL12 ocean color data processing system with the BMW option for the NIR reflectance correction algorithm
EUMETSAT/Jiang and Wang, 2014
This SeaWiFS image of our world depicts the global biosphere—the ocean’s long-term average phytoplankton chlorophyll concentration acquired between September 1997 and August 2000 combined with the SeaWiFS-derived Normalized Difference Vegetation Index over land during July 2000.
SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE
Sentinel-3 OLCI coccolithophore blooms
Phytoplankton swirl in the Atlantic ocean off the coast of Iceland on June 3, 2016. (NASA Worldview)
NASA
Provided by Ewa Kwiatowska
Schematic explaining the concept of the biological carbon pump – how phytoplankton contribute to take-up and storage of atmospheric carbon dioxide.
NOC / RAPID ABC Fluxes
http://www.rapid.ac.uk/abc/background.php
Sentinel-3 OLCI chlorophyll-a concentration early result
SeaWiFS Biosphere from 1997 to 2006
NASA
Sentinel-3 OLCI chlorophyll-a concentration early result. The dark blues have the lowest concentrations, followed by the light blues, then greens, yellow, and finally red which has the highest concentration of Chlorophyll a.
Provided by Ewa Kwiatowska
NASA Worldview