Arctic May Face Record Loss of Ozone This Spring

stratosphere clouds over Arctic
Stratospheric clouds above the Arctic. (Image credit: Ross J. Salawitch, University of Maryland)

Cold temperatures in the upper atmosphere and the lingering presence of ozone-destroying pollutants, called chlorofluorocarbons, have set the stage for what could be a record loss in protective ozone over the Arctic this spring.

"We have done everything to protect the atmosphere from CFCs (chlorofluorocarbons), still we get record ozone loses once in a while," said Markus Rex, an ozone researcher with the Alfred Wegener Institute for Polar and Marine Research in Germany.

"Right now, at the relevant altitude, we have lost about half of the ozone that should be there," Rex told

Rex and other researchers from Europe, Russia and North America came to this conclusion based on data collected by 30 stations in and slightly south of the Arctic.

The position of the polar vortex on March 14th, 2011, with air masses exposed to ozone loss colored in red. (Image credit: ECMWF/AWI-Potsdam)

Climate change connection?

Global warming is also a likely contributor. Scientists believe it is responsible for cooling the stratosphere, the layer of the atmosphere where the ozone layer is located, approximately 12.4 miles (20 kilometers) above the Earth's surface. By trapping heat lower down and warming the surface of the Earth, greenhouse gases actually cool the stratosphere. In recent years, the coldest of stratospheric winter temperatures have been getting colder, according to the researchers.  [Earth's Atmosphere: Top to Bottom]

This year, more ozone has been lost over the Arctic due to unusually cold temperatures in the stratosphere, and these have been fed by a stronger circulation pattern called the polar vortex throughout the winter, according to Ross Salawitch, a professor at the University of Maryland, and one of Rex's collaborators.

These polar clouds, which are composed of frozen nitric acid and sulfuric acid, form when temperatures in the stratosphere fall below minus 108 F (minus 78 C). This is currently the case in vast sections of the Arctic. Chemical processes on the surface of the cloud particles transform the initially harmless chemicals from chlorofluorocarbons (CFCs) into aggressive ozone-depleting substances. (Image credit: Markus Rex, Alfred Wegener Institute)

The air inside this vortex, which is created by a combination of cold temperatures over the pole and the rotation of the Earth, is much colder than the air outside. That cooling leads to cloud formation inside the vortex and the ensuing chemical reactions that produce highly reactive molecules with unpaired electrons. These, in turn, react with ozone, breaking apart its three oxygen atoms.

This is problematic because ozone blocks harmful radiation — which can damage DNA and lead to skin cancer, among other problems — from reaching the Earth's surface.

The same dynamics are responsible for the more infamous hole in the ozone above Antarctica. However, over the South Pole, the vortex circulation system is larger, stronger and more predictable from year to year, Salawitch said.

In 1987, under the Montreal Protocol, countries agreed to end production of ozone-destroying substances, including chlorofluorocarbons — but because they linger in the atmosphere, ozone losses aren't expected to end for the next 50 years or so, Rex said.

Within the next few decades, any cooling of the stratosphere connected to global warming can be expected to lead to large ozone loss, Rex said. The Earth's average surface temperature is estimated to have warmed 1.3 degrees Fahrenheit (0.7 degrees Celsius) since humans accelerated greenhouse gas emissions around the time of the Industrial Revolution.

Almost a record

The ozone depletion over the Arctic this year is neck and neck with the loss experienced in 2005. The arrival of the spring sun causes the vortex to dissipate, and this happened in mid to early March of 2005, according to the scientists.

"We expect that the record will soon be broken," Rex said. 

The remnants of the vortex — which contain the depleted ozone — typically pass overhead at about 45 to 50 degrees north latitude, over parts of Europe and North America, for a few days in spring, causing the potential for ultraviolet (UV) radiation exposure to increase, said Rex.

You can follow LiveScience writer Wynne Parry on Twitter @Wynne_Parry.

Wynne Parry
Wynne was a reporter at The Stamford Advocate. She has interned at Discover magazine and has freelanced for The New York Times and Scientific American's web site. She has a masters in journalism from Columbia University and a bachelor's degree in biology from the University of Utah.