Warmer is not always wetter
Compared to global warming caused by solar
radiation, global warming caused by greenhouse gases results in less
rainfall, simulations suggest
Not all warming is the
same. For the same increase in temperature, global warming caused by
greenhouse gases results in less rainfall than does warming caused by
the sun’s radiation, climate simulations suggest.
Because wet places should
get more rain as the climate heats up, the new results may explain
the mystery of why a warm period 1,000 years ago was wetter than the
warm late 20th century. Jian Liu of the Chinese Academy of Sciences
in Nanjing and colleagues describe these results in the Jan. 31
Nature.
“If what they show holds
up, it’s good news in that it helps reconcile an apparent
contradiction,” says oceanographer Gabriel Vecchi of the National
Oceanic and Atmospheric Administration’s Geophysical Fluid Dynamics
Laboratory in Princeton, N.J. But it would also limit how scientists
can use some past episodes of climate change as analogs for the
future, he says.
During the Medieval Warm
Period from 1000 to 1250, temperatures rose because the sun started
to release more radiation and there were few volcanic eruptions
spewing sun-blocking aerosols into the atmosphere. Climate
simulations indicate global precipitation was higher during this warm
spell than at the end of the 20th century, when temperatures
increased because of rising levels of carbon dioxide and other
greenhouse gases.
Liu and colleagues
investigated this rain disparity by simulating climate over the last
millennium, comparing the effects of solar radiation during
pre-industrial times with those of greenhouse gases during the
industrial period. For every one degree Celsius increase in
temperature, greenhouse gases boosted global rainfall by 1.2 to 1.3
percent. Meanwhile, solar warming caused a 2.1 percent increase in
rainfall.
These rainfall differences
may be a consequence, the researchers say, of how solar radiation and
greenhouse gases alter the distribution of heat in the atmosphere and
influence sea surface temperatures in the tropical Pacific Ocean —
factors that have a big effect on rainfall.
Warming of any kind
increases global rainfall by raising surface temperatures, the
researchers reason, and by increasing the difference in temperature
between Earth’s surface and the upper boundary of the lower
atmosphere. But greenhouse gas warming counteracts the effect
somewhat because the gases also trap heat in the atmosphere. The
result is a smaller heat difference than would result from solar
warming, the researchers say.
In turn, these heat
differences appear to affect temperatures in the Pacific. Normally,
the western Pacific is several degrees warmer than the eastern
Pacific. With solar warming, trade winds may strengthen and amplify
this temperature gradient. This leads to La NiƱa-like conditions in
which rainfall increases in already wet regions, thereby increasing
the total amount of rainfall on Earth. Fossil corals suggest a
temperature change like this may have occurred during the really wet
Medieval Warm Period, says study coauthor Mark Cane, a climate
scientist at Columbia’s Lamont-Doherty Earth Observatory in
Palisades, N.Y.
During greenhouse-gas
warming, the simulations indicate, the opposite trend in the Pacific
occurs: The temperature differential between the eastern and western
Pacific shrinks. This shifts normal rainfall patterns east, but
doesn’t lead to the same kind of rainfall intensification seen
during solar warming.
Cane
says the team needs to do much more work to really understand how
warming influences all of the mechanisms that interact to modify sea
surface temperatures in the Pacific and thus the Earth’s rainfall.
But the new findings already could influence attempts to mitigate
climate change, he says. If countries try to cool the planet by
somehow shielding it from incoming solar radiation, that won’t
reverse all of global warming’s changes. “We don’t have a way
of exactly undoing the effects of greenhouse gases,” he says.
No comments:
Post a Comment