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Arctic Melting Linked to Human Causes, Long-Term Review Finds


The dramatic loss of Arctic sea ice in recent years is the result of human-induced greenhouse gas emissions combined with natural cycles, according to a new study.

The loss of ice will likely change water temperatures and affect the circulation of ocean currents, which may alter climates around the world, the study suggests.

The study reviewed previous research of Arctic sea ice, which showed that the ice has been steadily disappearing since 1979.

In September 2005 satellite images revealed that the Arctic ice was at its lowest level in some 50 years of observation.

“If we compare how much ice we had in September 2005 with a typical September, we’ve lost an amount of ice about twice the size of Texas,” said lead author Mark Serreze, senior researcher at the National Snow and Ice Data Center at the University of Colorado, Boulder.

“So we’re talking about a lot of real estate.”

There have been previous periods of Arctic warmth not attributed to human causes, Serreze said, and ice cover grows each winter only to shrink in summer.

But the current loss probably can’t be ascribed to natural cycles alone, Serreze believes.

In the March 16 issue of the journal Science, Serreze and colleagues report that the evidence “strongly suggests” the ice loss is caused by human-induced global warming.

Natural Variations, Human Causes

The researchers pored over decades’ worth of satellite images, as well as records from airplanes and ships, to compile a historical picture of Arctic sea ice over the past half century.

The records show that the extent of sea ice fluctuates dramatically each year, reaching its low point in September before starting to grow once more with the onset of winter.

Arctic temperatures have also varied dramatically from decade to decade and were abnormally warm from 1925 to 1945, the data show.

But the most recent reports demonstrate that Arctic temperatures have increased at almost twice the global average rate over the past century.

Natural variations “play a large role” in the Arctic’s changing air temperature, Serreze said. But overall the observations are consistent with the melting that climate models have predicted would result from higher greenhouse-gas emissions.

“There has always been uncertainty about whether these observed changes are natural variability,” he said.

“But we now have a consensus between observations and what the models are telling us. In my mind, it’s very convincing that we’re starting to the see the effects of human activity on Arctic ice cover.”

Arctic Impact Goes Global

Human-caused warming may change the seasonal ice system and dramatically speed the loss of ice, said Bruno Tremblay of McGill University in Montreal, Canada, who was not involved in the new study.

“The system can recover from a low ice year. But, as warming continues, a critical thickness is reached beyond which the system no longer recovers,” he said.

Open water absorbs solar energy that would otherwise have been reflected by ice, he explained, which perpetuates the melting cycle.

“So ocean water warms, and the ice forms later in the fall, and you typically have an earlier melt onset,” he said.

Vanishing sea ice might also spur the melting of Greenland’s ice cap by warming the ocean waters into which the glaciers spill.

“In a place like Greenland the amount of heat that waters carry in summer is directly related to how much ice there would be,” said Ian Howat, a researcher with the University of Washington’s Polar Science Center who was not involved with the Science report.

“One can almost imagine sea ice acting like a buffer around the coast of Greenland. Remove that buffer, and the heat could more efficiently get at the edge of the ice sheet.”

No data exists to link shrinking sea ice cover with Greenland’s glaciers, Howat said, but he sees an intriguing correlation.

“It’s interesting that 2005 was the largest single loss of Arctic sea ice,” he said.

“The glaciers in Greenland retreated more in 2005 than we’ve ever seen them retreat. One of the major points of our research is that the glaciers are much more sensitive to short-term variability than we had previously thought.”

Weather Effects

Many scientists believe that the loss of sea ice may have significant impacts on the world’s climate.

The regions near Earth’s equator function as a sort of furnace for the planet’s climate system, while the Arctic acts as a kind of air conditioner by reflecting warming sunlight and cooling ocean waters. The two regions are intimately linked.

A loss of ice will likely change water temperatures and affect the circulation of ocean currents, altering regional climates, Serreze said.

“If you fundamentally change the nature of the Arctic, the rest of the system has to respond. The devil is in the details—what will those changes look like?” he asked.

Some models suggest reduced rainfall and increased droughts in the already arid western regions of North America.

The changes could also result in increased winter precipitation in western and southern Europe, as well as more intense storm tracks in the globe’s mid latitudes.

But climate modeling is so complex that no one really knows, Serreze pointed out.


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