Regional Changes in Carbon Dioxide Fluxes of Land and Oceans since 1980

We have applied an inverse model to 20 years of atmospheric carbon dioxide measurements to infer yearly changes in the regional carbon balance of oceans and continents. The model indicates that global terrestrial carbon fluxes were approximately twice as variable as ocean fluxes between 1980 and 199...

Full description

Saved in:
Bibliographic Details
Published inScience (American Association for the Advancement of Science) Vol. 290; no. 5495; pp. 1342 - 1346
Main Authors Bousquet, Philippe, Peylin, Philippe, Ciais, Philippe, Le Quéré, Corinne, Friedlingstein, Pierre, Tans, Pieter P.
Format Journal Article
LanguageEnglish
Published Washington, DC American Society for the Advancement of Science 17.11.2000
American Association for the Advancement of Science
The American Association for the Advancement of Science
American Association for the Advancement of Science (AAAS)
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:We have applied an inverse model to 20 years of atmospheric carbon dioxide measurements to infer yearly changes in the regional carbon balance of oceans and continents. The model indicates that global terrestrial carbon fluxes were approximately twice as variable as ocean fluxes between 1980 and 1998. Tropical land ecosystems contributed most of the interannual changes in Earth's carbon balance over the 1980s, whereas northern mid- and high-latitude land ecosystems dominated from 1990 to 1995. Strongly enhanced uptake of carbon was found over North America during the 1992-1993 period compared to 1989-1990.
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ObjectType-Article-1
ObjectType-Feature-2
ISSN:0036-8075
1095-9203
DOI:10.1126/science.290.5495.1342