Earth  ID: 208

Sea Surface Temperature-Phytoplankton Correlation around the Galapagos in May 1998

SeaWiFS documented the rapid demise of El Niño in the waters around the Galapagos Islands. The images show a explosion in plankton growth as the warm El Niño waters blamed for choking off essential ocean nutrients are replaced by deep cold upwelled waters. The false color images, which document plankton concentrations a period from May 9 to May 24, 1998, show that life in the region to the west archipelago has returned in remarkable abundance. High concentrations are shown red. Areas occluded by clouds are shown in white.

For More Information

http://svs.gsfc.nasa.gov/stories/elnino/index.html


Visualization Credits

Horace Mitchell (NASA/GSFC): Lead Animator
Marte Newcombe (GST): Animator
Gene Feldman (NASA/GSFC): Scientist
Please give credit for this item to:
NASA/Goddard Space Flight Center, The SeaWiFS Project and GeoEye, Scientific Visualization Studio. NOTE: All SeaWiFS images and data presented on this web site are for research and educational use only. All commercial use of SeaWiFS data must be coordinated with GeoEye (NOTE: In January 2013, DigitalGlobe and GeoEye combined to become DigitalGlobe).

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Data Used:
NOAA-14/AVHRR 1998/05/10, 1998/05/25
SeaStar/SeaWiFS/NDVI 1998/05/10, 1998/05/25
Note: While we identify the data sets used in these visualizations, we do not store any further details nor the data sets themselves on our site.

This item is part of this series:
El Niño and La Niña

Keywords:
DLESE >> Biological oceanography
DLESE >> Physical oceanography
SVS >> Phytoplankton
GCMD >> Location >> Galapagos Islands
NASA Science >> Earth

GCMD keywords can be found on the Internet with the following citation: Olsen, L.M., G. Major, K. Shein, J. Scialdone, S. Ritz, T. Stevens, M. Morahan, A. Aleman, R. Vogel, S. Leicester, H. Weir, M. Meaux, S. Grebas, C.Solomon, M. Holland, T. Northcutt, R. A. Restrepo, R. Bilodeau, 2013. NASA/Global Change Master Directory (GCMD) Earth Science Keywords. Version 8.0.0.0.0