(COMTEX) B: Climate: Earth brightens up ( United Press International )
BOULDER, Colo., May 16, 2005 (United Press International via COMTEX) -- The
25-year battle for clean air seems to be paying off in a brighter and possibly
warmer Earth.
There was a 4 percent to 6 percent decrease in the amount of solar radiation
reaching Earth's surface between the 1950s and the 1990s, said Chuck Long, a
senior scientist at the U.S. Department of Energy's Pacific Northwest National
Laboratory. Since 1990, however, solar energy reaching the surface has increased
about 4 percent.
Martin Wild, of the Institute for Atmospheric and Climate Science in Zurich, and
colleagues wrote in the May 6 issue of the journal Science that the Earth has
been brightening since at least the late 1980s. They do not state conclusively
it is the result of cleaning up emissions of dust and chemicals into the air,
but that is one strong contender.
"What caused it?" Long said rhetorically. "That's going to be complex to solve.
For that you need far more sophisticated measurements where you're making
long-term measurements of the cloud microphysical properties."
Ironically, U.S. and European success in reducing industrial and automotive air
pollution may be allowing more sunlight to reach the Earth, allowing the
greenhouse warming signal from the atmosphere to show up more clearly.
No one is certain of the cause of "global dimming," however. Other candidates
include changes in clouds, reaction to volcanic eruptions, and instrument
deficiencies.
Air pollution particles, atmospheric dust and other detritus in the air
generically are referred to as aerosols. These have a complex effect on climate,
sometimes absorbing sunlight before it reaches the surface, cooling things down.
Some particles, like black carbon emitted from smokestacks, tend to heat the
atmosphere.
In addition, these tiny particles can be the basis of cloud formation. Clouds,
in turn, have a complex and poorly understood impact on overall climate,
depending on the heights at which they form, how thick they are, how much water
vapor they contain, and so on.
When everything is factored in, though, aerosols tend to cool the atmosphere,
counteracting the global warming signal from carbon dioxide accumulation in the
atmosphere.
Lynn Russell, associate professor at the Scripps Institution of Oceanography at
the University of California-San Diego, and colleagues wrote last year they
found a net cooling effect of 0.5 watts per meter square -- a little greater
than current climates models incorporate.
If, in fact, the aerosols are declining and are responsible for the brightening
of the Earth, more sunlight may be absorbed by greenhouse gases in the
atmosphere, unmasking the climate signal that has been cooled by those aerosols.
Earth's atmosphere is heated from the bottom up, like a pot of water on a stove.
So if the amount of energy reaching the Earth increases, you would expect the
atmosphere to heat up.
As with all things climate related, there are dissenters. Fred Singer, a
physicist and president of the Science & Environmental Policy Project, wrote in
his weekly newsletter: "If these observations are correct, it means that the
greenhouse effect is smaller than required to account for the small warming
trend observed by weather satellites. Hence a smaller climate sensitivity and a
reduced temperature estimate for 2100, an increase of less than 0.5 Celsius (0.9
degrees Fahrenheit)."
Long noted, however, nothing they found challenges the scientific consensus on
global warming -- quite the contrary.
"It actually helps to, in a sense, clear up some of the mystery because people
have been asking the question. We know that for decades now we have been dumping
more carbon dioxide and stuff into the atmosphere. And we have been looking for
a warming trend, and it wasn't very obvious," Long told Climate. "That could be
because the solar dimming was masking it."
The effects of any change like this are complex and poorly understood. The
amount of heat reflected back to the atmosphere to heat it from the bottom up
depends on the Earth's reflectivity or its albedo. The overall albedo of the
Earth is very poorly understood.
In another paper in the same issue of Science, University of Washington
atmospheric scientist Robert Charlson and colleagues wrote, "Albedo changes may
be as important as changes in greenhouse gases for determining changes in global
climate."
The albedo cannot be measured directly. Methods to do so include measuring
"earthshine" -- the amount of light from Earth reflected by the moon --
satellite observations, ground cloud cover measurements and others.
The trouble is the variation of albedo measurements is large.
"In fact, the albedo change that is the equivalent of the enhanced greenhouse
effect is barely detectable by the available methods for measuring albedo," the
paper said.
The effect of aerosols on reflectivity are both direct and indirect, Casper
Ammann, a paleoclimatologist for the National Center for Atmospheric Research in
Boulder, told Climate. "If you have a whole bunch of aerosol and you start to
make clouds around them, what happens is that because you have more condensation
nuclei provided by these aerosols, the average cloud droplet size seems to be
smaller than if you do it under normal conditions."
Clouds with these smaller particles potentially can hang around longer.
"Quantification of the calculation of these indirect effects is extremely
complex," Ammann added.
Nothing in this work, however, suggests greenhouse warming is lessened.
"The moment that you stop or reduce the aerosol loads, this counter-effect is
diminished," Ammann said. "Therefore the greenhouse effect from the gases acts
more strongly, or shows its real face."
--
Climate is a weekly series examining the potential impact of global climate
change, by veteran environmental reporter Dan Whipple. E-mail:
sciencemail@upi.com
By DAN WHIPPLE
Copyright 2005 by United Press International.
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