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CHANGES IN OCEANIC AND TERRESTRIAL CARBON UPTAKE SINCE 1982
Author(s): FRANCEY RJ, TANS PP, ALLISON CE, ENTING IG, WHITE JWC, TROLIER M
Source: NATURE    Volume: 373    Issue: 6512    Pages: 326-330    Published: JAN 26 1995  
Times Cited: 302     References: 20     
Abstract: CHANCES in the carbon isotope ratio (delta(13)C) of atmospheric CO2 can be used in global carbon-cycle models(1-5) to elucidate the relative roles of oceanic and terrestrial uptake of fossil-fuel CO2. Here we present measurements of delta(13)C made at several stations in the Northern and Southern hemispheres over the past decade. Focusing on the highest-quality data from Cape Grim (41 degrees S), which also provide the longest continuous record, we observe a gradual decrease in delta(13)C from 1982 to 1993, but with a pronounced flattening from 1988 to 1990. There is an inverse relationship between CO2 growth rate(6) and El Nino/Southern Oscillation (ENSO) events which is not reflected in the isotope record. Thus, for the ENSO events in 1982, 1986 and 1991-92, we deduce that net ocean uptake of CO2 increased, whereas during La Nina events, when equatorial sea surface temperatures are lower, upwelling of carbon-rich water increases the release of CO2 from the oceans. The flattening of the trend from 1988 to 1990 appears to involve the terrestrial carbon cycle, but we cannot yet ascribe firm causes. We find that the large and continuing decrease in CO2 growth starting in 1988(6) involves increases in both terrestrial and oceanic uptake, the latter persisting through 1992.
Document Type: Article
Language: English
Reprint Address: FRANCEY, RJ (reprint author), CSIRO, DIV ATMOSPHER RES, PRIVATE BAG 1, MORDIALLOC, VIC 3195 AUSTRALIA
Addresses:
1. NOAA, CLIMATE MONITORING & DIAGNOST LAB, BOULDER, CO 80303 USA
2. UNIV COLORADO, DEPT GEOL SCI, BOULDER, CO 80309 USA
3. UNIV COLORADO, INST ARCTIC & ALPINE RES, BOULDER, CO 80309 USA
Publisher: MACMILLAN MAGAZINES LTD, 4 LITTLE ESSEX STREET, LONDON, ENGLAND WC2R 3LF
Subject Category: Multidisciplinary Sciences
IDS Number: QD404
ISSN: 0028-0836
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