For more information contact:

Rob Gutro
AGU Press Room Washington Convention Center May 28, 2002
(Phone: 202/371-5016)

Cynthia M. O'Carroll
Goddard Space Flight Center, Greenbelt, Md.
(Phone: 301/614-5563)

Charles Rose
University of Maryland Baltimore County
(Phone: 410/455-5793)

Caption for Image One: These grids depict the strength and shape of planetary-sized waves or long waves in both 1984 and 1997 in the northern mid-latitudes. These long waves affect the atmospheric circulation in the Arctic by strengthening it and warming temperatures, or weakening it and cooling temperatures. Warmer temperatures do not harm ozone, but colder temperatures cause the formation of polar clouds which convert chlorine to a reactive form that depletes ozone.

The ozone layer prevents the sun's harmful ultra-violet radiation from reaching the Earth's surface. Ultra-violet radiation is a primary cause of skin cancer. Without upper-level ozone, life on Earth might not exist. In 1984, the long waves were strong, as depicted by the solid black lines. The stronger waves provided the fuel for the atmospheric circulation to warm the stratosphere in the north polar region. Because the stratosphere was warm, reactive chlorine levels were low, and less ozone was lost. The orange and red colors represent high ozone levels present in the upper atmosphere. In 1997, the waves were weaker, as depicted by the broken black line. The weaker long waves provide little fuel for the atmospheric circulation that normally warms the polar stratosphere, making it colder than usual. Colder temperatures cause polar clouds to form, which lead to chemical reactions converting chlorine to a form that can deplete the ozone layer. The reduced ozone is depicted in the blue and purple.

Caption for Image Two: This diagram depicts the evolution of polar ozone at altitudes of 22-26 km, just above the level where polar stratospheric clouds (PSCs) typically form. During the fall, cooling over the pole causes descent of stratospheric air, bringing down air with higher levels of ozone. In a year with an early sudden warming, horizontal transport of air with even higher levels of ozone may dominate the air motions, leading to especially high ozone levels in the vortex. From early to late winter, cooling continues over the pole resulting in continued descent. Anomalously high ozone levels at 22-26 km can be carried by the descent to lower levels in the stratosphere (20 km), an altitude where PSCs may form. The difference in ozone levels at the end of winter, shown by the red and blue lines, represents differences due to both interannual variation in transport and losses on PSCs. The difference between the red ozone level and the dashed green one below it represents the difference due to transport variability alone.

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May 28, 2002 - (date of web publication)

A WARM POLAR WINTER WAS EASIER ON ARCTIC OZONE

	Image 1

A NASA researcher has found unusually high levels of protective upper atmospheric ozone in the Arctic as a result of a rare sudden warming during the early winter of 1998.

"There are several factors that control polar ozone including air temperature in the stratosphere, the presence of polar stratospheric clouds (PSCs), and the timing and strength of large atmospheric waves that bring ozone to the poles from the tropics," said Susan Strahan, an atmospheric scientist at NASA's Goddard Space Flight Center, Greenbelt, Md., and author of a paper being presented at the American Geophysical Union's spring meeting in Washington.

	Image 2

During the wintertime, as the temperatures drop, winds swirl around the poles and form a vortex. The atmospheric circulation brings ozone from the upper to the lower stratosphere, where temperatures are colder. The stronger the vortex, the less ozone is transported to the cold lower stratosphere, where breakdown of ozone by PSCs can occur.

During 1998, however, Strahan found that more low latitude air surged poleward in December of that year bringing higher levels of ozone than usual and warmer than normal temperatures into the Arctic vortex. From January to March, the high ozone air descended to lower altitudes in the vortex, where polar stratospheric clouds often form. These clouds form during colder temperatures and cause ozone molecules to break apart, but the warm air that surged with the ozone prevented the PSCs from forming.

"As a result, ozone in the lower stratospheric vortex was higher than usual this year because more ozone than usual was transported into it," Strahan said.

Strahan's research is supported by earlier findings by NASA's Paul Newman in 2001 that said large-scale atmospheric waves carry ozone from the equator to the poles. Typically, ozone "piles up" in the stratosphere over the tropics. When the large-scale waves are stronger and occur more often than usual, they push more low latitude air northward, bringing high ozone and warmer temperatures with them to the poles.

According to Newman, "In cold years like 1997, weaker, and less frequent waves reduced the effectiveness of the Arctic heat engine and cooled the stratosphere, making conditions just right for ozone destruction."

Strahan explained that in a cold year, with weaker waves, polar ozone levels get a "double whammy," because less ozone gets transported to the poles from the tropics because temperatures are lower, allowing more PSCs form, which leads to more ozone loss.

Strahan said that it is important to keep in mind that even without ozone loss by PSCs, the amount of ozone in the Arctic stratosphere varies from year to year depending on the strength of the large-scale waves and the quantity of ozone they bring. Further, she stressed that ozone loss by chlorine is controlled by temperature and only indirectly by the variability in the large-scale waves.

If the wave activity is strong enough to raise the vortex above temperatures where the PSCs can form throughout the winter, then the wave activity can prevent ozone loss. She said that December 1999 had little wave activity, allowing the Arctic vortex to become large and strong by the beginning of winter. This restricted the transport of ozone to the polar region, while at the same time, the low vortex temperatures allowed a significant amount of PSCs to form and more ozone loss to occur during the winter of 1999 to 2000.

This research was funded under NASA's Earth Science Enterprise, Atmospheric Chemistry Modeling and Analysis Program (ACMAP).

Strahan will present this paper, "The Influence of Planetary Wave Transport on Arctic Ozone as Observed by POAM III" at the American Geophysical Union Spring 2002 meeting at the Washington Convention Center in Washington, D.C., on Tuesday, May 28, 2002, at 9:30 a.m., Session A21E-05, Room WCC20.

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