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The Chatham Rise, an underwater plateau that stretches from the South
Island of New Zealand to beyond the Chatham Islands,
separates two areas of deeper water to the north and south. (Tides and
other currents flowing over this submarine topography enhance vertical
mixing in the water column. That mixing and the location of the rise
along the subtropical front (where cold currents from the Antarctic meet
warmer, subtropical waters) foster large blooms of phytoplankton in the
area, especially in the Southern Hemisphere spring and summer.
Like plants on land, phytoplankton are the foundation of the marine
food web, using sunlight to convert atmospheric carbon dioxide and water
into the carbohydrate glucose. All other marine life-from squid, to
fish, to whales-depend directly or indirectly on phytoplankton, which
makes tracking the size and frequency of phytoplankton blooms important
to biologists monitoring the health of our oceans.
Phytoplankton also influence and are influenced by the climate.
Phytoplankton remove the same amount of the greenhouse gas carbon
dioxide from the air as land plants do, helping to counter global
warming. But warming of the oceans appears to be responsible for a global
decline in phytoplankton productivity over the past decade.
This image was captured by the Moderate Resolution Imaging
Spectroradiometer (MODIS) on
NASA's Aqua satellite, which has been
monitoring ocean
chlorophyll and other of Earth's vital signs since 2002.
NASA image by Norman Kuring, Ocean Color Team. Caption by
Norman Kuring and Rebecca Lindsey. A version of the image with
bathymetry contours is available on the Ocean Color Team Website.
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