NASA Research Reveals Climate Warming Reduces Ocean Food Supply

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Dec. 6, 2006

Erica Hupp/Dwayne Brown
Headquarters, Washington 
202-358-1237/1726 

Rob Gutro
Goddard Space Flight Center, Greenbelt, Md.
301-286-4044 

RELEASE: 06-364

NASA RESEARCH REVEALS CLIMATE WARMING REDUCES OCEAN FOOD SUPPLY

WASHINGTON - In a NASA study, scientists have concluded that when 
Earth's climate warms, there is a reduction in the ocean's primary 
food supply. This poses a potential threat to fisheries and 
ecosystems. 

By comparing nearly a decade of global ocean satellite data with 
several records of Earth's changing climate, scientists found that 
whenever climate temperatures warmed, marine plant life in the form 
of microscopic phytoplankton declined. Whenever climate temperatures 
cooled, marine plant life became more vigorous or productive. The 
findings will appear in the journal Nature on Dec. 7. 

The results provide a preview of what could happen to ocean biology in 
the future if Earth's climate warms as the result of increasing 
levels of greenhouse gases in the atmosphere. 

"The evidence is pretty clear that the Earth's climate is changing 
dramatically, and in this NASA research we see a specific consequence 
of that change," said oceanographer and study co-author Gene Carl 
Feldman of NASA's Goddard Space Flight Center, Greenbelt. Md. "It is 
only by understanding how climate and life on Earth are linked that 
we can realistically hope to predict how the Earth will be able to 
support life in the future."

Phytoplankton are microscopic plants living in the upper sunlit layer 
of the ocean. They are responsible for approximately the same amount 
of photosynthesis each year as all land plants combined. Changes in 
phytoplankton growth and photosynthesis influence fishery yields, 
marine bird populations and the amount of carbon dioxide the oceans 
remove from the atmosphere.

"Rising levels of carbon dioxide in the atmosphere play a big part in 
global warming," said lead author Michael Behrenfeld of Oregon State 
University, Corvallis. "This study shows that as the climate warms, 
phytoplankton growth rates go down and along with them the amount of 
carbon dioxide these ocean plants consume. That allows carbon dioxide 
to accumulate more rapidly in the atmosphere, which would produce 
more warming."

The findings are from a NASA-funded analysis of data from the 
Sea-viewing Wide Field-of-view Sensor (SeaWiFS) instrument on the 
OrbView-2 spacecraft, launched in 1997. SeaWiFS is jointly operated 
by GeoEYE, Dulles, Va. and NASA.

The uninterrupted nine-year record shows in great detail the ups and 
downs of marine biological activity or productivity from month to 
month and year to year. Captured at the start of this data record was 
a major, rapid rebound in ocean biological activity after a major El 
Nino event. El Nino and La Nina are major warming or cooling events, 
respectively, that occur approximately every 3-7 years in the eastern 
Pacific Ocean and are known to change weather patterns around the 
world.

Scientists made their discovery by comparing the SeaWiFS record of the 
rise and fall of global ocean plant life to different measures of 
recent global climate change. The climate records included several 
factors that directly effect ocean conditions, such as changes in sea 
surface temperature and surface winds. The results support computer 
model predictions of what could happen to the world's oceans as the 
result of prolonged future climate warming.

"When we compared changes in phytoplankton activity with simultaneous 
changes in climate conditions, the agreement between the two records 
was simply astonishing," Behrenfeld said.

Ocean plant growth increased from 1997 to 1999 as the climate cooled 
during one of the strongest El Ni?o to La Ni?a transitions on record. 
Since 1999, the climate has been in a period of warming that has seen 
the health of ocean plants diminish.

The new study also explains why a change in climate produces this 
effect on ocean plant life. When the climate warms, the temperature 
of the upper ocean also increases, making it "lighter" than the 
denser cold water beneath it. This results in a layering or 
"stratification" of ocean waters that creates an effective barrier 
between the surface layer and the nutrients below, cutting off 
phytoplankton's food supply. The scientists confirmed this effect by 
comparing records of ocean surface water density with the SeaWiFS 
biological data.

For information about NASA and agency programs on the Internet, visit: 


http://www.nasa.gov

	
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