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Reply Wed 7 Apr, 2004 06:50 pm
Illustration by Monica Seaberry
SCIENCE AND TECHNOLOGY

Disputed `Global Dimming' Evidence Gaining Currency Among Scientists

BY MARGIE WYLIE
c.2004 Newhouse News Service

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More stories by Margie Wylie


Gerald Stanhill was reviewing solar radiation records in the late 1980s when he stumbled onto something that amazed him: Days were growing dimmer.

"It was difficult to believe," said Stanhill, an Israeli government scientist. "So I started looking around for other continuous, long series of solar radiation measurements to make sure it wasn't an error."

It wasn't. Since 1973, he found, scientific papers had documented downward trends in surface solar radiation in Japan, the Soviet Union and Germany, among other places.

Stanhill, in about a dozen papers beginning in 1992, went on to detail declines in Israel, Australia, Hong Kong, Ireland and even the Arctic and Antarctic. In 1998, researchers at the Swiss Federal Institute of Technology published a 30-year analysis that found a 10 percent average drop, but at sites concentrated in the Northern Hemisphere.

Then, in 2001, emeritus biologist Stanhill of Israel's Agricultural Research Organization and agency colleague Shabtai Cohen published a study of all available evidence. They found surface solar radiation had dropped an average 3 percent per decade since the late 1950s. In all, sunlight had plummeted more than 10 percent worldwide between 1958 and 1992.

Stanhill called the phenomenon "global dimming."

A dramatic drop in sunshine could have implications for everything from solar energy to plant growth, but its main impact may be on how we understand man-made climate change, or global warming. Indeed, many climate scientists who read the 2001 paper either ignored it or insisted -- given that global dimming seemed to run counter to the overall warming trend -- that the measurements had to be wrong.

"It's very difficult to explain how there can be a substantial reduction in solar radiation at the Earth's surface and at the same time a substantial increase in the temperature," Stanhill said.

As a result, said Veerabhadran Ramanathan, an atmospheric scientist with Scripps Institute of Oceanography in La Jolla, Calif., "many took the easy route to just disbelieve it."

Then came the work of Graham Farquhar and Michael Roderick at Australian National University in Canberra.

For years, researchers had been puzzled by a steady, worldwide decrease in the amount of water that evaporates from open pans, despite the Earth's rising temperatures. Farquhar, a plant physiologist, and Roderick, an ecologist, came up with an explanation.

They compared 50 years of evaporation measurements to Stanhill's solar radiation measurements, and got a match. Less sunlight was hitting the water's surface, they reasoned, resulting in less surface heat and thus less evaporation.

For solar power generation, the consequences of global dimming are obvious: Less sunshine falling on solar cells generates less electricity.

For plant growth, the consequences are murkier, scientists say. Even though less sunlight is reaching plants, a greater fraction of that light is scattered, which can be beneficial. "I think it's a bit of an open question what (global dimming) does for photosynthesis," Farquhar said.

Farquhar and Roderick published their results in the prestigious journal Science in 2002, giving global dimming a toehold in the wider scientific world. The topic has gained enough currency to merit a special session at the joint meeting of the American and Canadian geophysical unions in Montreal this May.

What causes global dimming? Scientists think smoky pollution plays a big part.

Tiny particles suspended in the atmosphere can reflect or absorb incoming sunlight before it reaches the ground. This promotes formation of bigger, more persistent and more reflective clouds that less readily condense into rain, said Beate G. Liepert, an atmospheric physicist at Columbia University's Lamont-Doherty Earth Observatory in Palisades, N.Y.

Industrialized regions have dimmed the most. For example, Israel's coastal plain now gets 30 percent less solar radiation than 50 years ago, Stanhill said. Ramanathan found that vast brown hazes generated in Asia and hanging over the Indian Ocean and the Himalayas can cut surface sunlight by as much as 30 percent.

A worrisome possibility, Liepert said, is that at least some of the decrease in sunshine is connected to the warming caused by greenhouse gases. Unlike particulates, these gases don't wash out of the air in a matter of days once cars and factories stop spewing them out.

"Hot air can hold more water," she said -- and under hotter conditions, you get more and thicker clouds.

Add up the effect of particulates, greenhouse gases and reduced evaporation and what global dimming might be telling us is that we're in for an even hotter, drier future than previously anticipated from global warming, both Liepert and Ramanathan said.

With only 35 years of data, some researchers aren't ready to go that far.

"It's an interesting phenomenon, but maybe it's a bit premature to call it global," said Martin Wild, a climatologist at the Swiss Federal Technical Institute in Zurich. "We have no idea what's going on over the oceans, which cover 70 percent of the Earth."

Nor do scientists know how long global dimming has been going on or whether it will last. Researchers are still analyzing records from the last decade. There are early indications that the phenomenon may have eased as pollution controls were taking effect.

In Germany, for example, University of South Carolina researcher Helen Power found that sunlight levels rose several years after many heavy industries were shuttered. Power warns that her study was limited and offers no conclusive answers.

To detect trends before the late 1950s, when standardized solar radiation measurements became widespread, Stanhill and Cohen are combing through 125 years of sunshine duration records. They will present their findings at the meeting in May.

Whatever the answer, Stanhill, who has been emeritus since 1994, can at last actually retire. "I'm feeling that I can safely leave it all to others now," he said.

March 31, 2004


(Margie Wylie can be contacted at [email protected])
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Type: Discussion • Score: 1 • Views: 1,050 • Replies: 6
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neil
 
  1  
Reply Wed 7 Apr, 2004 07:51 pm
1 In 50 years the instruments, recording protocol and other details likely have evolved to account for part of the dimming 2 the sun may have dimmed 3 some fundamental law of physics may have changed. Perhaps lots of things are changing slightly. On another thread we tentatively determined that no one is checking to see if the atmosphere still averages 21 % oxygen. Neil
0 Replies
 
cicerone imposter
 
  1  
Reply Wed 7 Apr, 2004 08:02 pm
neil, I thought it only interesting. I don't buy into this kind of thesis, because we don't know if they are normal cycles of this planet - somewhat similar to global warming.
0 Replies
 
littlek
 
  1  
Reply Wed 7 Apr, 2004 08:08 pm
fascinating!
0 Replies
 
fishin
 
  1  
Reply Wed 7 Apr, 2004 08:23 pm
Hmmm.. Verra verra interesting. Wink
0 Replies
 
cicerone imposter
 
  1  
Reply Wed 7 Apr, 2004 08:26 pm
It's still 21% according to this article.
********
"Astronomy 161: Dr. Eric Monier
Thursday, August 7

EARTH'S ATMOSPHERE



--------------------------------------------------------------------------------

KEY IDEAS
The Earth's atmosphere consists mainly of nitrogen and oxygen.
Without life, the air would have no O2; without oceans, it would have more CO2.
The Earth has a magnetic field, generated by currents in the outer core.

--------------------------------------------------------------------------------

(1) The Earth's atmosphere consists mainly of nitrogen (N2) and oxygen (O2).

The Earth's atmosphere is 78% nitrogen, 21% oxygen, 1% argon and contains trace amounts of water, carbon dioxide, etc.
The air pressure is about 15 pounds per square inch at sea level, and decreases steadily with altitude. At the 9 km (29,000 feet) altitude of Mt. Everest, the air pressure is 1/3 that at sea level. There is no clear boundary to the Earth's atmosphere; the atmospheric pressure drops steadily with altitude until the atmosphere blends with tenuous interplanetary gas.
Temperature does not necessarily decrease steadily with altitude. It is customary to divide the atmosphere into four layers:

Troposphere (0 to 12 kilometers above surface)
temperature decreases with altitude (as you climb Everest, you get colder).
Stratosphere (12 to 50 km)
temperature increases with altitude, warmed by ozone absorbing
ultraviolet light from the Sun.
Mesosphere (50 to 80 km)
temperature decreases with altitude.
Thermosphere (80 km to ???)
temperature increases with altitude; the thermosphere is warmed by the absorption of very high
energy ultraviolet and x-ray photons."
0 Replies
 
Eos
 
  1  
Reply Thu 8 Apr, 2004 09:17 pm
I would think it would have to do with the increased amount of particulate pollution in the atmosphere (smog, dust from the erosion caused by land-clearing). Any thoughts?
0 Replies
 
 

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