k Falsecolour satellite images of the Atlantic Ocean in winter and in spring, showing the seasonal changes in phytoplankton distribution. The colours represent varying phytoplankton densities from red most dense through yellow, green and blue to violet least dense. Land areas are coloured grey and regions where no measurements were possible are coloured black. The increase in sunlight during the spring causes a phytoplankton bloom which covers the entire North Atlantic. The image was produced from data acquired by the Coastal Zone Colour Scanner on NASAs Nimbus7 research satellite. Editorial Stock Photo - Afloimages
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False-colour satellite images of the Atlantic Ocean in winter and in spring, showing the seasonal changes in phytoplankton distribution. The colours represent varying phytoplankton densities from red (most dense) through yellow, green and blue to violet (least dense). Land areas are coloured grey and regions where no measurements were possible are coloured black. The increase in sunlight during the spring causes a phytoplankton bloom which covers the entire North Atlantic. The image was produced from data acquired by the Coastal Zone Colour Scanner on NASA's Nimbus-7 research satellite.
ED

False-colour satellite images of the Atlantic Ocean in winter and in spring, showing the seasonal changes in phytoplankton distribution. The colours represent varying phytoplankton densities from red (most dense) through yellow, green and blue to violet (least dense). Land areas are coloured grey and regions where no measurements were possible are coloured black. The increase in sunlight during the spring causes a phytoplankton bloom which covers the entire North Atlantic. The image was produced from data acquired by the Coastal Zone Colour Scanner on NASA's Nimbus-7 research satellite.

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ID
10576117

Collection

License type
Editorial

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Creation date
16-11-2010

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