Global Climate Change Digest: Main Page | Introduction | Archives | Calendar | Copy Policy | Abbreviations | Guide to Publishers

GCRIO Home ->arrow Library ->arrow Archives of the Global Climate Change Digest ->arrow September 1998 ->arrow PROFESSIONAL PUBLICATIONS... ATMOSPHERIC CHEMISTRY AND DYNAMICS Search

U.S. Global Change Research Information Office logo and link to home

Last Updated:
February 28, 2007

GCRIO Program Overview



Our extensive collection of documents.


Get Acrobat Reader

Privacy Policy

Global Climate Change DigestArchives of the
Global Climate Change Digest

A Guide to Information on Greenhouse Gases and Ozone Depletion
Published July 1988 through June 1999



Item #d98sep9

“Mass-Independent Oxygen Isotope Fractionation in Atmospheric CO as a Result of the Reaction CO + OH,” T. Röckmann et al.,Science 281, 544-546 (July 24, 1998).

Atmospheric CO exhibits isotope-fractionation effects that are not related to the mass of the substituted isotope. Excess 17O was detected in atmospheric CO at high northern latitudes during the summer. This excess 17O ranged up to 7.5o/oo. The excess results from the reaction CO + OH ® CO2 + H, which is the most common reaction of CO in the atmosphere. The surviving CO exhibits the excess, meaning that the reaction with OH demonstrates a preference for CO with 18O over that with 17O, raising fundamental questions about the kinetic processes involved. No theoretical explanation is known to explain this selective process. A similar effect also occurs in the formation of ozone, where the reaction 16O + 18O18O occurs 50% more readily than the reaction 18O + 16O16O. The anomaly does make the concentration of C17O a good marker for the age of CO in the atmosphere.

Item #d98sep10

“Seasonal Cycles and QBO Variations in Stratospheric CH4 and H2O Observed in UARS HALOE Data,” W. J. Randel et al., J. Atmos. Sci. 55 (2), 163-185 (1998).

Stratospheric methane and water vapor were measured from 1991 to 1997 during the Halogen Occultation Experiment that employed the Upper Atmosphere Research Satellite. The data reveal latitudinal gradients in atmospheric mixing in the subtropics and across the polar vortices. They indicate a strong descent inside the polar vortices during winter and spring. And they show a strong seasonal upwelling in the tropical upper atmosphere associated with the semiannual oscillation. All of these findings are in agreement with the processes of the mean meridional circulation as understood from stratospheric meteorological analyses. Most of the variance in interannual variations is related to the equatorial quasibiennial oscillation, which also affects the latitudinal position of the tropical “reservoir” in the middle atmosphere.

  • Guide to Publishers
  • Index of Abbreviations

  • Hosted by U.S. Global Change Research Information Office. Copyright by Center for Environmental Information, Inc. For more information contact U.S. Global Change Research Information Office, Suite 250, 1717 Pennsylvania Ave, NW, Washington, DC 20006. Tel: +1 202 223 6262. Fax: +1 202 223 3065. Email: Web: Webmaster:
    U.S. Climate Change Technology Program Intranet Logo and link to Home