期刊
SCIENCE
卷 351, 期 6274, 页码 696-699出版社
AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.aac4971
关键词
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资金
- European Union [283080, 242316, 283201]
- U.S. Department of Energy [DE-SC0012167]
- NSF [1304270]
- NOVA [UID/AMB/04085/2013]
- U.S. Department of Energy (DOE) [DE-SC0012167] Funding Source: U.S. Department of Energy (DOE)
- Directorate For Geosciences
- Office of Polar Programs (OPP) [1304270] Funding Source: National Science Foundation
Atmospheric monitoring of high northern latitudes (above 40 degrees N) has shown an enhanced seasonal cycle of carbon dioxide (CO2) since the 1960s, but the underlying mechanisms are not yet fully understood. The much stronger increase in high latitudes relative to low ones suggests that northern ecosystems are experiencing large changes in vegetation and carbon cycle dynamics. We found that the latitudinal gradient of the increasing CO2 amplitude is mainly driven by positive trends in photosynthetic carbon uptake caused by recent climate change and mediated by changing vegetation cover in northern ecosystems. Our results underscore the importance of climate-vegetation-carbon cycle feedbacks at high latitudes; moreover, they indicate that in recent decades, photosynthetic carbon uptake has reacted much more strongly to warming than have carbon release processes.
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