MODIS Sea Surface Temperature Data Shows Increased Temperatures in Southern Great Barrier Reef

  • Released Thursday, March 17, 2005
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Coral bleaching may be one of the greatest threats to the Great Barrier Reef. Coral bleaching is a stress response that often occurs when the surrounding waters become too warm for the corals. In the stressful situation, the corals expel their brownish zooxanthellae and lose their color. Zooxanthellae are unicellular yellow-brown algae that make it possible for the corals to grow and reproduce quickly enough to create reefs. Without the zooxanthellae, the coral cannot obtain sufficient nourishment. If conditions remain difficult, the corals may die. Major coral bleaching incidents on the Great Barrier Reef in 1998 and 2002 led to widespread death of corals in some areas. Researchers in the Barrier reef of Australia are using NASA's resources to help identify troubled coral. Currently, the most severe coral bleaching occurs over inshore reefs where the Sea Surface Temperatures are showing increased temperatures.

Sea Surface Temperature Colortable

Sea Surface Temperature Colortable

Herron Island is in the southern Great Barrier Reef and is part of the Capricorn Group of Islands, just off of the Capricorn Coast.

Herron Island is in the southern Great Barrier Reef and is part of the Capricorn Group of Islands, just off of the Capricorn Coast.

 This is an IKONOS image of coral bleaching around Herron Island in the Great Barrier Reef.

This is an IKONOS image of coral bleaching around Herron Island in the Great Barrier Reef.



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NASA/Goddard Space Flight Center Scientific Visualization Studio

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This page was originally published on Thursday, March 17, 2005.
This page was last updated on Wednesday, May 3, 2023 at 1:56 PM EDT.


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