Movatterモバイル変換


[0]ホーム

URL:


Skip to main page content
U.S. flag

An official website of the United States government

Dot gov

The .gov means it’s official.
Federal government websites often end in .gov or .mil. Before sharing sensitive information, make sure you’re on a federal government site.

Https

The site is secure.
Thehttps:// ensures that you are connecting to the official website and that any information you provide is encrypted and transmitted securely.

NIH NLM Logo
Log inShow account info
Access keysNCBI HomepageMyNCBI HomepageMain ContentMain Navigation
pubmed logo
Advanced Clipboard
User Guide

Full text links

Springer full text link Springer
Full text links

Actions

Share

Review
.2022 May;65(5):861-895.
doi: 10.1007/s11427-021-2045-5. Epub 2022 Feb 8.

Terrestrial carbon sinks in China and around the world and their contribution to carbon neutrality

Affiliations
Review

Terrestrial carbon sinks in China and around the world and their contribution to carbon neutrality

Yuanhe Yang et al. Sci China Life Sci.2022 May.

Abstract

Enhancing the terrestrial ecosystem carbon sink (referred to as terrestrial C sink) is an important way to slow down the continuous increase in atmospheric carbon dioxide (CO2) concentration and to achieve carbon neutrality target. To better understand the characteristics of terrestrial C sinks and their contribution to carbon neutrality, this review summarizes major progress in terrestrial C budget researches during the past decades, clarifies spatial patterns and drivers of terrestrial C sources and sinks in China and around the world, and examines the role of terrestrial C sinks in achieving carbon neutrality target. According to recent studies, the global terrestrial C sink has been increasing from a source of (-0.2±0.9) Pg C yr-1 (1 Pg=1015 g) in the 1960s to a sink of (1.9±1.1) Pg C yr-1 in the 2010s. By synthesizing the published data, we estimate terrestrial C sink of 0.20-0.25 Pg C yr-1 in China during the past decades, and predict it to be 0.15-0.52 Pg C yr-1 by 2060. The terrestrial C sinks are mainly located in the mid- and high latitudes of the Northern Hemisphere, while tropical regions act as a weak C sink or source. The C balance differs much among ecosystem types: forest is the major C sink; shrubland, wetland and farmland soil act as C sinks; and whether the grassland functions as C sink or source remains unclear. Desert might be a C sink, but the magnitude and the associated mechanisms are still controversial. Elevated atmospheric CO2 concentration, nitrogen deposition, climate change, and land cover change are the main drivers of terrestrial C sinks, while other factors such as fires and aerosols would also affect ecosystem C balance. The driving factors of terrestrial C sink differ among regions. Elevated CO2 concentration and climate change are major drivers of the C sinks in North America and Europe, while afforestation and ecological restoration are additionally important forcing factors of terrestrial C sinks in China. For future studies, we recommend the necessity for intensive and long term ecosystem C monitoring over broad geographic scale to improve terrestrial biosphere models for accurately evaluating terrestrial C budget and its dynamics under various climate change and policy scenarios.

Keywords: carbon cycle; carbon neutrality; carbon sink; global warming; terrestrial ecosystem.

© 2022. Science China Press and Springer-Verlag GmbH Germany, part of Springer Nature.

PubMed Disclaimer

Similar articles

See all similar articles

Cited by

See all "Cited by" articles

References

    1. Adams, J.M., Faure, H., Faure-Denard, L., McGlade, J.M., and Woodward, F.I. (1990). Increases in terrestrial carbon storage from the Last Glacial Maximum to the present. Nature 348, 711–714. - DOI
    1. Ahlström, A., Raupach, M.R., Schurgers, G., Smith, B., Arneth, A., Jung, M., Reichstein, M., Canadell, J.G., Friedlingstein, P., Jain, A.K., et al. (2015). The dominant role of semi-arid ecosystems in the trend and variability of the land CO2 sink. Science 348, 895–899. - PubMed - DOI
    1. Ajtay, G.L., Ketner, P., and Duvigneaud, P. (1979). Terrestrial primary production and phytomass. In: Bolin, B., Degens, E.T., Kempe, S., and Ketner, P., eds. The Global Carbon Cycle. Chichester: John Wiley & Sons. 129–181.
    1. Arora, V.K., and Melton, J.R. (2018). Reduction in global area burned and wildfire emissions since 1930s enhances carbon uptake by land. Nat Commun 9, 1326. - PubMed - PMC - DOI
    1. Baccini, A., Walker, W., Carvalho, L., Farina, M., Sulla-Menashe, D., and Houghton, R.A. (2017). Tropical forests are a net carbon source based on aboveground measurements of gain and loss. Science 358, 230–234. - PubMed - DOI

Publication types

MeSH terms

Substances

Related information

LinkOut - more resources

Full text links
Springer full text link Springer
Cite
Send To

NCBI Literature Resources

MeSHPMCBookshelfDisclaimer

The PubMed wordmark and PubMed logo are registered trademarks of the U.S. Department of Health and Human Services (HHS). Unauthorized use of these marks is strictly prohibited.


[8]ページ先頭

©2009-2025 Movatter.jp