Elvidge and others produced the map of the contiguous states to see how
urban sprawl is affecting the planet's budget of carbon, a greenhouse gas
when it is in the form of carbon dioxide.
"As you add pavement, buildings and sidewalks, you are decreasing the area
that can have vegetation," Elvidge said. "With that, you're decreasing the
uptake of carbon by plants."
Ironically, there are some cases where the paving of America results in an
increase of plants that take up more carbon dioxide, Elvidge said. Golf
courses and lawns in some desert communities have changed the carbon balance
there.
"Phoenix is like an oasis with a barren desert around it," he said. "In some
cases, lawns take up much more carbon than the original vegetation that
would have been there."
The transformation from wilderness to city has also created "heat islands,"
where blacktop and heat-absorbing shingles make cities warmer than the
surrounding countryside. Los Angeles, for example, is about 7 degrees
Fahrenheit warmer than areas around it. Even Fairbanks is a heat island,
with winter temperatures downtown up to 20 degrees warmer than outlying
areas.
Elvidge said scientists who study Earth's carbon equation are not the only
ones who are interested in the new map of the United States' non-absorbent
surfaces. Hydrologists want the information to help them model flood
potential. Other groups use the nighttime lights data to detect large fires,
to monitor activity in fisheries where fishermen use bright lights to
attract fish, to check where people are burning natural gas flares off oil
wells, to find the best place is to set up a telescope for star gazing, and
even to locate good habitat for sea turtles, which thrive on beaches with
little or no artificial light.
When the worldwide map of impervious surfaces is complete, Elvidge said he
expects to find a few countries with a higher percentage of developed land
than the U.S.
"One I'm sure of is Singapore," he said. "And maybe some European
countries."
He and his colleagues are sure of another thing
This column is provided as a public service by the Geophysical Institute,
University of Alaska Fairbanks, in cooperation with the UAF research
community. Ned Rozell is a science writer at the institute. This column
first appeared in 2004.
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