Amplified Greenhouse Effect Shifts North's Growing Seasons

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March 10, 2013

Steve Cole 
Headquarters, Washington 
202-358-0918 
stephen.e.cole@xxxxxxxx 

Kathryn Hansen 
Goddard Space Flight Center, Greenbelt, Md. 
301-286-1046 
kathryn.h.hansen@xxxxxxxx 

Ruth Marlaire 
Ames Research Center, Moffett Field, Calif. 
650-604-4709 
ruth.marlaire@xxxxxxxx 

RELEASE: 13-069

AMPLIFIED GREENHOUSE EFFECT SHIFTS NORTH'S GROWING SEASONS

WASHINGTON -- Vegetation growth at Earth's northern latitudes 
increasingly resembles lusher latitudes to the south, according to a 
NASA-funded study based on a 30-year record of land surface and newly 
improved satellite data sets. 

An international team of university and NASA scientists examined the 
relationship between changes in surface temperature and vegetation 
growth from 45 degrees north latitude to the Arctic Ocean. Results 
show temperature and vegetation growth at northern latitudes now 
resemble those found 4 degrees to 6 degrees of latitude farther south 
as recently as 1982. 

"Higher northern latitudes are getting warmer, Arctic sea ice and the 
duration of snow cover are diminishing, the growing season is getting 
longer and plants are growing more," said Ranga Myneni of Boston 
University's Department of Earth and Environment. "In the north's 
Arctic and boreal areas, the characteristics of the seasons are 
changing, leading to great disruptions for plants and related 
ecosystems." 

The study was published Sunday in the journal Nature Climate Change. 

Myneni and colleagues used satellite data to quantify vegetation 
changes at different latitudes from 1982 to 2011. Data used in this 
study came from NOAA's Advanced Very High Resolution Radiometers 
(AVHRR) onboard a series of polar-orbiting satellites and NASA's 
Moderate Resolution Imaging Spectroradiometer (MODIS) instruments on 
the Terra and Aqua satellites. 

As a result of enhanced warming and a longer growing season, large 
patches of vigorously productive vegetation now span a third of the 
northern landscape, or more than 3.5 million square miles (9 million 
square kilometers). That is an area about equal to the contiguous 
United States. This landscape resembles what was found 250 to 430 
miles (400 to 700 kilometers) to the south in 1982. 

"It's like Winnipeg, Manitoba, moving to Minneapolis-Saint Paul in 
only 30 years," said co-author Compton Tucker of NASA's Goddard Space 
Flight Center in Greenbelt, Md. 

The Arctic's greenness is visible on the ground as an increasing 
abundance of tall shrubs and trees in locations all over the 
circumpolar Arctic. Greening in the adjacent boreal areas is more 
pronounced in Eurasia than in North America. 

An amplified greenhouse effect is driving the changes, according to 
Myneni. Increased concentrations of heat-trapping gasses, such as 
water vapor, carbon dioxide and methane, cause Earth's surface, ocean 
and lower atmosphere to warm. Warming reduces the extent of polar sea 
ice and snow cover, and, in turn, the darker ocean and land surfaces 
absorb more solar energy, thus further heating the air above them. 

"This sets in motion a cycle of positive reinforcement between warming 
and loss of sea ice and snow cover, which we call the amplified 
greenhouse effect," Myneni said. "The greenhouse effect could be 
further amplified in the future as soils in the north thaw, releasing 
potentially significant amounts of carbon dioxide and methane." 

To find out what is in store for future decades, the team analyzed 17 
climate models. These models show that increased temperatures in 
Arctic and boreal regions would be the equivalent of a 20-degree 
latitude shift by the end of this century relative to a period of 
comparison from 1951-1980. 

However, researchers say plant growth in the north may not continue on 
its current trajectory. The ramifications of an amplified greenhouse 
effect, such as frequent forest fires, outbreak of pest infestations 
and summertime droughts, may slow plant growth. 

Also, warmer temperatures alone in the boreal zone do not guarantee 
more plant growth, which also depends on the availability of water 
and sunlight. 

"Satellite data identify areas in the boreal zone that are warmer and 
dryer and ¬¬other areas that are warmer and wetter," said co-author 
Ramakrishna Nemani of NASA's Ames Research Center in Moffett Field, 
Calif. "Only the warmer and wetter areas support more growth." 
Researchers did find found more plant growth in the boreal zone from 
1982 to 1992 than from 1992 to 2011, because water limitations were 
encountered in the latter two decades. 

Data, results and computer codes from this study will be made 
available on NASA Earth Exchange (NEX), a collaborative 
supercomputing facility at Ames. NEX is designed to bring scientists 
together with data, models and computing resources to accelerate 
research and innovation and provide transparency. 

For more information and images associated with this release, visit: 

http://go.nasa.gov/12Amv2s 

	
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