期刊
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
卷 106, 期 28, 页码 11496-11501出版社
NATL ACAD SCIENCES
DOI: 10.1073/pnas.0902930106
关键词
clumped isotopes; CO2; mesosphere; polar vortex; stratosphere
资金
- Davidow Fund (California Institute of Technology)
- National Science Foundation
- National Aeronautics and Space Administration Upper Atmosphere Research Program
- Camille Dreyfus Teacher- Scholar Award
The stratospheric CO2 oxygen isotope budget is thought to be governed primarily by the O(D-1)+CO2 isotope exchange reaction. However, there is increasing evidence that other important physical processes may be occurring that standard isotopic tools have been unable to identify. Measuring the distribution of the exceedingly rare CO2 isotopologue (OCO)-O-16-C-13-O-18, in concert with O-18 and O-17 abundances, provides sensitivities to these additional processes and, thus, is a valuable test of current models. We identify a large and unexpected meridional variation in stratospheric (OCO)-O-16-C-13-O-18, observed as proportions in the polar vortex that are higher than in any naturally derived CO2 sample to date. We show, through photochemical experiments, that lower (OCO)-O-16-C-13-O-18 proportions observed in the midlatitudes are determined primarily by the O(D-1)+CO2 isotope exchange reaction, which promotes a stochastic isotopologue distribution. In contrast, higher (OCO)-O-16-C-13-O-18 proportions in the polar vortex show correlations with long-lived stratospheric tracer and bulk isotope abundances opposite to those observed at midlatitudes and, thus, opposite to those easily explained by O(D-1)+CO2. We believe the most plausible explanation for this meridional variation is either an unrecognized isotopic fractionation associated with the mesospheric photochemistry of CO2 or temperature-dependent isotopic exchange on polar stratospheric clouds. Unraveling the ultimate source of stratospheric (OCO)-O-16-C-13-O-18 enrichments may impose additional isotopic constraints on biosphere-atmosphere carbon exchange, biosphere productivity, and their respective responses to climate change.
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