National Aeronautics and Space Administration Logo
Follow this link to skip to the main content NASA Banner
Solar System Exploration
News & Events
NASA Spacecraft Measures Unusual 2005 Artic Ozone Conditions
NASA Spacecraft Measures Unusual 2005 Artic Ozone Conditions
2 Jun 2005
(Source: Jet Propulsion Laboratory)

Alan Buis (818) 354-0474
Jet Propulsion Laboratory, Pasadena, Calif.

News Release: 2005-092 June 2, 2005

NASA Spacecraft Measures Unusual 2005 Arctic Ozone Conditions

Despite near-record levels of chemical ozone destruction in the Arctic this winter,
observations from NASA's Aura spacecraft showed that other atmospheric processes
restored ozone amounts to near average and stopped high levels of harmful ultraviolet
radiation from reaching Earth's surface.

Analyses from Aura's Microwave Limb Sounder indicated Arctic chemical ozone destruction
this past winter peaked at near 50 percent in some regions of the stratosphere, a region of
Earth's atmosphere that begins about 8 to 12 kilometers (5 to 7 miles) above Earth's poles.
This was the second highest level ever recorded, behind the 60 percent level estimated for
the 1999-2000 winter. Data from another instrument on Aura, the Ozone Monitoring
Instrument, found the total amount of ozone over the Arctic this past March was similar to
other recent years when much less chemical ozone destruction occurred. So what
tempered the ozone loss? The answer appears to lie in this year's unusual Arctic
atmospheric conditions.

"This was one of the most unusual Arctic winters ever," said scientist Dr. Gloria Manney of
NASA's Jet Propulsion Laboratory, Pasadena, Calif., who led the Microwave Limb Sounder
analyses. "Arctic lower stratospheric temperatures were the lowest on record. But other
conditions like wind patterns and air motions were less conducive to ozone loss this year."

While the Arctic polar ozone was being chemically destroyed toward the end of winter,
stratospheric winds shifted and transported ozone-rich air from Earth's middle latitudes into
the Arctic polar region, resulting in little net change in the total amount of ozone. As a
result, harmful ultraviolet radiation reaching Earth's surface remained at near-normal levels.

Imagery and an animation depicting the Microwave Limb Sounder and Ozone Monitoring
Instrument 2005 Arctic ozone observations may be viewed at:

http://www.nasa.gov/vision/earth/lookingatearth/ozone-aura.html .

Extensive ozone loss occurs each winter over Antarctica (the "ozone hole") due to the
extreme cold there and its strong, long-lived polar vortex (a band of winds that forms each
winter at high latitudes). This vortex isolates the region from middle latitudes. In contrast,
the Arctic winter is warmer and its vortex is weaker and shorter-lived. As a result, Arctic
ozone loss has always been lower, more variable and much more difficult to quantify.

This was the first Arctic winter monitored by Aura, which was launched in July 2004. Aura's
Microwave Limb Sounder is contributing to our understanding of the processes that cause
Arctic wind patterns to push ozone-rich air to the Arctic lower stratosphere from higher
altitudes and lower latitudes. Through Aura's findings, scientists can differentiate chemical
ozone destruction from ozone level changes caused by air motions, which vary dramatically
from year to year.

"Understanding Arctic ozone loss is critical to diagnosing the health of Earth's ozone layer,"
said Dr. Phil DeCola, Aura program scientist at NASA Headquarters, Washington.
"Previous attempts to quantify Arctic ozone loss have suffered from a lack of data. With
Aura, we now have the most comprehensive, simultaneous, global daily measurements of
many of the key atmospheric gases needed to understand and quantify chemical ozone
destruction."

Ozone loss in Earth's stratosphere is caused primarily by chemical reactions with chlorine
from human-produced compounds like chlorofluorocarbons. When stratospheric
temperatures drop below minus 78 degrees Celsius (minus 108 degrees Fahrenheit), polar
stratospheric clouds form. Chemical reactions on the surfaces of these clouds activate
chlorine, converting it into forms that destroy ozone when exposed to sunlight.

The data obtained by Aura were independently confirmed by instruments participating in
NASA's Polar Aura Validation Experiment, which flew underneath Aura as it passed over
the polar vortex. The experiment, flown on NASA's DC-8 flying laboratory from NASA's
Dryden Flight Research Center, Edwards, Calif., carried 10 instruments to measure
temperatures, aerosols, ozone, nitric acid and other gases. The experiment was carried out
in January and February 2005.

Aura is the third and final major Earth Observing System satellite. Aura carries four
instruments: the Ozone Monitoring Instrument, built by the Netherlands and Finland in
collaboration with NASA; the High Resolution Dynamics Limb Sounder, built by the United
Kingdom and the United States; and the Microwave Limb Sounder and Tropospheric
Emission Spectrometer, both built by JPL. Aura is managed by NASA's Goddard Space
Flight Center, Greenbelt, Md.

For more information on Aura on the Internet, visit:

http://aura.gsfc.nasa.gov/ .

For more information on the Microwave Limb Sounder on the Internet, visit:

http://mls.jpl.nasa.gov/ .

JPL is managed for NASA by the California Institute of Technology in Pasadena.

News Archive Search  Go!
Show  results per page
 
 
Awards and Recognition   Solar System Exploration Roadmap   Contact Us   Site Map   Print This Page
NASA Official: Kristen Erickson
Advisory: Dr. James Green, Director of Planetary Science
Outreach Manager: Alice Wessen
Curator/Editor: Phil Davis
Science Writer: Autumn Burdick
Producer: Greg Baerg
Webmaster: David Martin
> NASA Science Mission Directorate
> Budgets, Strategic Plans and Accountability Reports
> Equal Employment Opportunity Data
   Posted Pursuant to the No Fear Act
> Information-Dissemination Policies and Inventories
> Freedom of Information Act
> Privacy Policy & Important Notices
> Inspector General Hotline
> Office of the Inspector General
> NASA Communications Policy
> USA.gov
> ExpectMore.gov
> NASA Advisory Council
> Open Government at NASA
Last Updated: 3 Jun 2005