For Immediate Release
December 2, 1999
Contacts: Lee Tune, 301 405 4679 or ltune@umd.edu
Science Team Finds That Humans Probably Are Contributing to Retreat of Arctic Sea Ice
COLLEGE PARK, MD For the first time, scientists have placed satellite-derived observations
of recent reductions in Arctic sea ice into a much longer-term context to show that sea ice
decreases probably are due, at least in part, to human-caused climate change and that substantial
decreases will probably continue in the future.
The findings, by a team of meteorologists, physicists, and climatologists from the
University of Maryland, Rutgers University, NOAA, the University of Illinois, NASA, the
Hadley Center in Great Britain, and the Arctic and Antarctic Research Institute in Russia, will
appear in the December 3 issue of Science.
The team, led by Konstantin Vinnikov of the University of Maryland's department of
meteorology, used computer climate models to examine whether the decreases observed in the
ice cover of the Arctic over the past few decades are the result exclusively of natural climate
changes or might also be influenced by human-induced global warming. First, observed satellite
and ground-based data were used to measure the retreat of Arctic sea ice. Then the team used a
computer model to simulate the changes in Arctic sea ice that would occur over 5,000-years of
natural variation in climate if there was no human-added carbon dioxide in the atmosphere.
"Satellite data shows that from November 1978 through March 1998 there was an overall
downward trend of 37,000 square kilometers per year in the extent of Arctic ice," said Vinnikov,
a senior research scientist at Maryland. "Our computer modeling shows a less than 2 percent
probability that natural variations in climate would produce such a large decrease over a period
of only 19.4 years, suggesting that the negative trend is due to more than just natural variability."
The science team also examined outputs from computer simulations that include human-
produced increases in carbon dioxide and aerosols. Carbon dioxide increases tend to warm the
atmosphere, while aerosol increases tend to cool the atmosphere. The models that include these
human-induced changes show a much better match with the observed sea ice decreases than the
model simulating natural variability alone.
This suggests that melting Arctic sea ice is probably related to human-induced global
warming, and that future decreases in sea ice extent can be predicted with some confidence using
models that contain human-induced atmospheric changes, the scientists say.
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