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Tropospheric Ozone Impacts Global Climate Warming - Cartesian Dissolve

In the first 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 (the troposphere) changed temperatures over the past 100 years. Using the best available estimates of global emissions of gases that create 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.

Ozone was responsible for one-third to half of the observed warming trend in the Arctic during winter and spring, according to the new research. Ozone is transported from the industrialized countries in the Northern Hemisphere to the Arctic quite efficiently during these seasons. The findings will be published soon in the American Geophysical Union's Journal of Geophysical Research-Atmospheres.

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, the 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 research was supported by NASA's Atmospheric Chemistry Modeling and Analysis Program.


This animation dissolves between anomalous temperature averages from December through May in  1880, 1950, and 1990.    This animation dissolves between anomalous temperature averages from December through May in 1880, 1950, and 1990.
Duration: 18.0 seconds
Available formats:
  720x486 (29.97 fps) Frames
  320x216     PNG           59 KB
  160x80       PNG           21 KB
  80x40         PNG           6 KB
  720x480 (29.97 fps) MPEG-2   16 MB
  640x480 (29.97 fps) MPEG-4   2 MB
  640x480 (29.97 fps) MPEG-1   3 MB
  320x240 (29.97 fps) MPEG-1   1 MB
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Temperature Colorbar
   Temperature Colorbar

Available formats:
  320 x 90           PNG   8 KB


 1880 - This image shows a decadal seasonal average between December through May in the years 1880 through 1889.    1880 - This image shows a decadal seasonal average between December through May in the years 1880 through 1889.

Available formats:
  2560 x 1920     TIFF 2 MB
  320 x 240         PNG 65 KB


 1950 - This  decadal winter and spring seasonal  average exposes slightly higher then normal temperatures in the Northern Hemisphere.    1950 - This decadal winter and spring seasonal average exposes slightly higher then normal temperatures in the Northern Hemisphere.

Available formats:
  2560 x 1920     TIFF 3 MB
  320 x 240         PNG 72 KB


 1990 - This  decadal winter and spring seasonal  average illustrates warmer then normal average temperatures in the northern latitudes.    1990 - This decadal winter and spring seasonal average illustrates warmer then normal average temperatures in the northern latitudes.

Available formats:
  2560 x 1920     TIFF 3 MB
  320 x 240         PNG 73 KB

Animation Number:3339
Animator:Lori Perkins (Lead)
Studio:SVS
Completed:2006-02-15
Scientist:Drew Shindell (NASA/GSFC GISS)
Writer:Steve Cole (SSAI)
Data set:Atmospheric Chemistry Modeling and Analysis Program: Anomalous Temperature Data
Data Collected:December through May for years 1880, 1950, and 1990
Series:Troprospheric Ozone Impact on Climate Warming
Keywords:
GCMD >> EARTH SCIENCE >> Climate Indicators >> Air Temperature Indices
GCMD >> EARTH SCIENCE >> Atmosphere >> Atmospheric Chemistry/Oxygen Compounds >> Ozone
 
 
Please give credit for this item to
NASA/Goddard Space Flight Center Scientific Visualization Studio


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