NASA scientists have found that a major form of global air pollution
involved in summertime "smog" has also played a significant role in warming
the Arctic.
In a global assessment of the impact of ozone on climate warming,
scientists at the NASA Goddard Institute for Space Studies (GISS), New York,
evaluated how ozone in the lowest part of the atmosphere changed
temperatures over the past 100 years. Using the best available estimates of
global emissions of gases that produce ozone, the GISS computer model study
reveals how much this single air pollutant, and greenhouse gas, has
contributed to warming in specific regions of the world.
According to this new research,
ozone was responsible for one-third to half of the observed warming trend
in the Arctic during winter and spring. Ozone is transported from the
industrialized countries in the Northern Hemisphere to the Arctic quite
efficiently during these seasons. The findings have been accepted for
publication in the American Geophysical Union's Journal of Geophysical
Research-Atmospheres.
Ozone plays several different roles in the Earth’s atmosphere. In the
high-altitude region of the stratosphere, ozone acts to shield the planet
from harmful ultraviolet radiation. In the lower portion of the atmosphere
(the troposphere), ozone can damage human health, crops and ecosystems.
Ozone is also a greenhouse gas and contributes to global warming.
Ozone is formed from several other chemicals found in the atmosphere near
the Earth's surface that come from both natural sources and human
activities such as fossil fuel burning, cement manufacturing, fertilizer
application and biomass burning. Ozone is one of several air pollutants
regulated in the United States by the U. S. Environmental Protection
Agency.
The impact of ozone air pollution on climate warming is difficult to
pinpoint because, unlike other greenhouse gases such as carbon dioxide,
ozone does not last long enough in the lower atmosphere to spread
uniformly around the globe. Its warming impact is much more closely tied
to the region it originated from. To capture this complex picture, GISS
scientists used a suite of three-dimensional computer models that starts
with data on ozone sources and then tracks how ozone chemically evolved
and moved around the world over the past century.
The warming impact of low-altitude ozone on the Arctic is very small in
the summer months because ozone from other parts of the globe does not
have time to reach the region before it is destroyed by chemical reactions
fueled by ample sunshine. As a result, when it is summertime in the
Northern Hemisphere, ozone-induced warming is largest near the sources of
ozone emissions. The computer model showed large summer warming from ozone
over western North America and eastern Europe/central Asia, areas with
high levels of ozone pollution during that time of year.
The new results identify an unexpected benefit of air pollution control
efforts worldwide, according to lead author Drew Shindell. "We now see
that reducing ozone pollution can not only improve air quality but also
have the added benefit of easing climate warming, especially in the
Arctic."
The research was supported by NASA’s Atmospheric Chemistry Modeling and
Analysis Program.
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