Antarctic Ozone Hole at Near Record Size This Year
Large size due to cold temperatures
Cold temperatures over Antarctica this year have resulted in an ozone "hole" that is the second largest ever observed,
according to U.S. scientists. The ozone hole is caused by ozone-depleting chemicals from human activity.
According to an October 7 press release, researchers report that the observed size of the ozone depletion region in 2003
is strikingly larger than the hole in 2002, the size of which was considered a quirk of meteorological conditions over
Antarctica due to warmer-than-normal stratospheric temperatures. The difference in the size of the ozone hole is
directly attributed to year-to-year temperature variations, not an increase in the amount of ozone-depleting compounds
in the atmosphere.
"In colder years, the same amount of ozone-depleting compounds can destroy more ozone, in comparison to warmer years,"
said Daniel Albritton, director of the Aeronomy Laboratory at the National Oceanic and Atmospheric Administration.
According to measurements by balloon instruments, the size of this year's Antarctic ozone hole reached 28.3 million
square kilometers on September 11, smaller than September 10, 2000, the largest ever hole recorded when it covered 29.9
million kilometers. Last year the ozone hole was smaller, covering 21 million square kilometers.
The ozone layer blocks harmful ultraviolet rays that have been linked to skin cancer in humans and other adverse
biological effects on plants and animals.
Chlorine and bromine-containing compounds from human activity are the primary cause of ozone hole, which is defined as a
thinning of the ozone layer to levels significantly below those seen prior to 1979. While the 1987 Montreal Protocol and
subsequent amendments sharply curtailed the use of these compounds, scientists say the chemicals will remain active in
the atmosphere for several decades. The ozone hole is expected to recover in about 50 years.
Following is the text of the press release:
National Oceanic and Atmospheric Administration
October 7, 2003
2003 ANTARCTIC OZONE ‘HOLE' NEAR RECORD SIZE; COLD TEMPERATURES PLAY MAJOR ROLE
This year's Antarctic ozone "hole" is the second largest ever observed, according to scientists from the National
Oceanic and Atmospheric Administration (NOAA), NASA, and the Naval Research Laboratory.
The size of the ozone depletion region shows an increase in its total size from last year, further indicating that the
relatively smaller hole of 2002 was mostly a quirk of meteorological conditions over Antarctica. The difference is
directly attributed to year-to-year temperature variations across the Antarctic continent, not an increase in the amount
of ozone-depleting compounds in the atmosphere.
"We expect to see year-to-year variations in the size of the ozone hole, because stratospheric temperatures can vary
from year to year. In colder years, the same amount of ozone-depleting compounds can destroy more ozone, in comparison
to warmer years," said Daniel L. Albritton, director of the NOAA Aeronomy Laboratory in Boulder, Colo.
The Antarctic ozone "hole" is defined as thinning of the springtime ozone layer to levels significantly below those seen
prior to 1979. Extreme cold in the upper atmosphere is one key factor that affects the amount of ozone loss caused by
ozone-depleting compounds. Year-to-year changes in the size and amount of depletion in the vertical column of the ozone
hole are dominated by the year-to-year variations in temperature in this part of the atmosphere.
Chlorine- and bromine-containing compounds from human activity are the primary cause of ozone depletion. The 1987 United
Nations Montreal Protocol and its subsequent amendments sharply curtailed the use of chlorine-containing
chlorofluorcarbons (CFCs) and bromine-containing halons. Because of the protocol, the amounts of these ozone-depleting
substances have begun to decline in the lower atmosphere and to level off in the stratosphere, where the ozone layer
"Although international protocols have greatly reduced the production and release of ozone depleting chemicals, they
will remain active in the stratosphere for several decades," said James Laver, Director of NOAA's Climate Prediction
Center. "With the protective atmospheric layer so compromised, greater amounts of ultraviolet radiation may be allowed
to reach the surface and potentially increase certain health risks." NOAA provides predictions of expected levels of
ultraviolet radiation in support of the Environmental Prediction Agency‘s Sunwise program.
At South Pole Station, balloon-borne ozone-measuring instruments launched by NOAA's Climate Monitoring and Diagnostics
Laboratory reveal the vertical structure of the developing ozone hole. An important gauge for identifying when future
recovery of the Antarctic ozone hole begins is the severity of depletion observed in the upper atmosphere near the main
Ozone measured by a balloon instrument on Sept. 26 showed nearly complete ozone destruction in the 9-13 mile altitude
layer. Total column ozone indicated a 60 per cent drop from early August measurements.
"This year, ozone depletion over the South Pole, from 7-to-14 miles above Antarctica, has shown large losses, similar to
losses seen in the 1990s," said Bryan Johnson of NOAA's Climate Monitoring and Diagnostics Laboratory.
Ozone blocks harmful ultraviolet "B" rays. Prolonged over-exposure to ultraviolet radiation has been linked to skin
cancer in humans and other adverse biological effects on plants and animals. The dramatic ozone "hole" exists only over
Antarctica, but currently, the ozone layer over the United States is depleted by about 6 percent.
Temperature over the Antarctic affects the formation of polar stratospheric clouds, which accelerate the destruction of
stratospheric ozone by human-produced chlorine and bromine compounds. The Antarctic ozone hole is still expected to
recover in about 50 years, when the atmospheric amounts of reactive chlorine and bromine return to their pre-ozone-hole
The observed size of the ozone depletion region in 2003 is a stark contrast from 2002. The reduced size in 2002 was
attributed to warmer-than-normal stratospheric temperatures and temperature patterns above Antarctica. The size of this
year's Antarctic ozone hole reached 10.9 million square miles on Sept. 11, 2003, smaller than Sept. 10, 2000, the
largest ever recorded when it covered 11.5 million square miles. Last year the ozone hole was smaller, covering 8.1
million square miles.
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more about NOAA, please visit: http://www.noaa.gov.
For more information on ozone research, please visit: http://www.ozonelayer.noaa.gov