Scientists: global warming is
causing spreading drought
Posted Jan. 12, 2005
Courtesy the National Science Foundation
and World Science staff
The percentage of Earth’s land area
stricken by serious drought more than doubled from the 1970s to the early
2000s, and global warming seems be a major reason, scientists announced this
week.
The researchers, with the
National Center for Atmospheric Research in Boulder, Colo., said widespread
drying occurred over much of Europe and Asia, Canada, western and southern
Africa.
Aiguo Dai, a scientist with the
center, presented the findings on Jan. 12 the American Meteorological Society
annual meeting in San Diego, Calif. The work also appeared in a paper published
in the December issue of the Journal of Hydrometeorology.
“The results reconfirm
the complexity of the climate system,” said Cliff Jacobs, program director in
division of atmospheric sciences of the National Science Foundation, U.S.A.
“We need to continue to develop a wide variety of research tools to understand
these changes.”
Dai and his colleagues found
that the fraction of global land experiencing very dry conditions rose from
about 10-15 percent in the early 1970s to about 30 percent by 2002. Almost half
of that change is due to rising temperatures rather than decreases in rainfall
or snowfall, according to Dai.
“These results point to
increased risk of droughts as human activity contributes to global warming,”
says Dai.
Even as drought has expanded
across Earth’s land areas, the amount of water vapor in the air has increased
over the past few decades, the researchers said. Average global precipitation
has also risen slightly. However, as Dai noted, “surface air temperatures over
global land areas have increased sharply since the 1970s.”
The large warming increases the
tendency for moisture to evaporate from land areas. Together, the overall area
experiencing either very dry or very wet conditions could occupy a greater
fraction of Earth’s land areas in a warmer world, Dai says.
“Droughts and floods are
extreme climate events that are likely to change more rapidly than the average
climate,” says Dai. “Because they are among the world’s costliest natural
disasters and affect a very large number of people each year, it is important to
monitor them and perhaps predict their variability.”
Dai and colleagues used
long-term records of temperature and precipitation from a variety of sources to
estimate soil moisture for the period 1870–2002. The results were consistent
with those from a historical computer simulation of global land surface
conditions. By factoring out rainfall and snowfall, Dai and colleagues estimated
how much of the changes moisture changes were due solely to rising temperatures.
“The warming-induced drying
has occurred over most land areas since the 1970s,” says Dai, “with the
largest effects in northern mid- and high latitudes.” In contrast, rainfall
deficits alone were the main factor behind expansion of dry soils in Africa’s
Sahel and East Asia. These are regions where El Niño, a more frequent visitor
since the 1970s, tends to inhibit rainfall.
Though most of the Northern
Hemisphere has shown a drying trend in recent decades, the United States has
bucked that trend, becoming wetter overall during the past 50 years, says Dai.
The trend is especially notable between the Rocky Mountains and Mississippi
River. Other parts of the world showing a moistening trend include Argentina and
parts of western Australia. These trends are related more to increased
precipitation than to temperature, says Dai.
“Global climate models
predict increased drying over most land areas during their warm season,” Dai
said. This occurs because of a general increase in “greenhouse gases,” such
as carbon dioxide, which trap heat in the atmosphere, he added. “Our analyses
suggest that this drying may have already begun.”
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