
Study Looks At Irrigation's
Impact on Regional Climate Change
Columbia
Basin
Bulletin
August 17, 2007
Expansion of irrigation
has masked greenhouse warming in
California
's
Central Valley
, but irrigation may not
make much of a difference in the future, according to a new study in the
Aug. 13 edition of the Proceedings of the National Academy of Sciences.
Irrigation's influence on
climate is often overlooked when studying the human effect on regional
climate change. Yet, irrigation has expanded rapidly in many parts of
the world and understanding its influence helps to explain historical
trends and to improve climate projections in those regions.
"Globally we derive
40 percent of our food from irrigated regions, so we'd like to be able
to model future climate changes in these regions," said Celine
Bonfils, lead author of the study from Lawrence Livermore National
Laboratory and U.C. Merced.
Based on observations of
temperature and irrigation trends throughout the state, the authors
demonstrated a clear irrigation-induced cooling in agricultural areas,
and showed that this effect has recently slowed down.
"This is not a model
result, but something very clearly evident in the data. We also looked
at other major irrigated regions in the world, and saw a very similar
pattern" Bonfils said.
The team, which included
Bonfils and David Lobell at Livermore Lab, first studied the net impact
of widespread irrigation on local and regional climate in
California
, the top irrigating state
in the
United States
(3.3 million hectares). In
highly irrigated regions of the
San Joaquin
Valley
, daytime temperatures
relative to low irrigated areas have cooled by 1.8 degrees - 3.2 degrees
C since the introduction of irrigation practice in 1887.
"In comparison,
there was no clear effect of irrigation on temperatures over the
1980-2000 period when there was no net growth of irrigation,"
Lobell said.
Irrigation cools the
surface of the earth by increasing the amount of energy used to
evaporate water rather than heat the land. The more irrigated the land,
the more intense the effect.
"It was quite
surprising how well we could distinguish a cooling trend that
incrementally increases with the amount of irrigation," Bonfils
said.
This study also shows
that the rapid summer nighttime warming, well observed in central
California
since 1915, cannot be
explained by irrigation expansion, as outside research has implied.
"Our results show that the expansion of irrigation has almost no
effect on minimum temperatures and that irrigation cannot be blamed for
this rapid warming," Bonfils said.
"An increase in
greenhouse gases and urbanization would best explain this trend, which
exceeds what is possible from natural climate variability alone,"
Lobell said.
In other areas of the
world where irrigation development has been rapid, including Thailand,
the Aral Sea Basin and Nebraska (the second most irrigated state in the
United States), the research team found the same cooling effect in
summer daytime maximum temperatures. In India, Pakistan and Eastern
China, the temperature change due to irrigation is a little less clear
because of the presence of aerosols in the atmosphere that also
contribute to the observed cooling by reflecting or absorbing sunlight.
In
California
, irrigation expansion is
likely to end because of urbanization and water demand increase. In the
United States
, irrigation has for the
first time decreased by 2 percent from 1998-2003 and growth in
irrigation has already slowed down in many parts of the world.
"Throughout the
major irrigated regions of the world, the cooling influence of
irrigation on daytime maximum temperatures will be much smaller in the
next 50 years than in the past century, and will likely not continue to
curb the effects of greenhouse warming anymore," Bonfils said.
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