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Decomposing the global carbon balance pressure index: evidence from 77 countries

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Abstract

Understanding the relationship between carbon emissions and vegetation carbon sequestration is essential for reducing the greenhouse effect. In this study, we constructed a carbon balance pressure index to measure the eco-environment pressure caused by carbon emissions in 77 countries from 2000 to 2015, and the logarithmic mean Divisia index decomposition method was used to identify the key factors related to carbon balance pressure. As the change in vegetation carbon sequestration is relatively stable, carbon emissions have become the direct cause of the rise in the global carbon balance pressure. The carbon balance pressure in advanced economies decreased slowly, while that in emerging economies increased but the growth rate decreased. The decomposition results showed that carbon intensity is the main factor restraining the rise of carbon balance pressure, while GDP per capita and land population pressure are the main driving forces, and vegetation carbon sequestration intensity plays only a small role. Further analysis showed that the restraining effect of carbon intensity can offset the incremental effect of GDP per capita in advanced economies, and the vegetation carbon sequestration intensity also has a positive impact, but not in emerging economies. Besides, different factors play different roles depending on the country. The conclusions were also supported by various robustness tests.

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Data availability

The datasets used during the current study are available from the corresponding author on reasonable request.

Notes

  1. BP Statistical Review of World Energy, available from https://www.bp.com/en/global/corporate/energy-economics/statistical-review-of-world-energy.html.

  2. World Bank Open Data, available from https://data.worldbank.org.

  3. Food and Agriculture Organization of the United Nations, available from http://www.fao.org/.

  4. NPP Data, available from https://lpdaac.usgs.gov/products/mod17a3v055.

  5. Environmental Performance Index 2018, available from https://sedac.ciesin.columbia.edu/data/set/epi-environmental-performance-index-2018.

  6. IMF-World Economic Outlook 2019, available from https://www.imf.org/en/Publications/WEO/Issues/2019/10/01/world-economic-outlook-october-2019.

  7. WMO, the global climate in 2011–2015, available from https://public.wmo.int/en.

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Funding

This study was supported by the Major Program of the National Social Science Foundation of China (Grant No. 20ZDA084); the National Natural Science Foundation of China (Grant Nos. 71934001, 71471001, 41771568, 71533004); the National Key Research and Development Program of China (Grant No. 2016YFA0602500); the Strategic Priority Research Program of Chinese Academy of Sciences (Grant No. XDA23070400); and the Sichuan Province Social Science High Level Research Team Building.

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Authors and Affiliations

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Contributions

Jiandong Chen: writing–original draft, funding acquisition, formal analysis; Zhiwen Li: writing–review and editing, investigation, software; Malin Song: writing–review and editing, funding acquisition, supervision, validation, project administration; Yizhe Dong: writing–review and editing, methodology, conceptualization, data curation. All authors read and approved the final manuscript.

Corresponding author

Correspondence to Malin Song.

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The authors declare that they have no competing interests.

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Responsible editor: Nicholas Apergis

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Appendices

Appendix A

Based on Eq. (4), CBPI was decomposed again according to the Laspeyres decomposition method, as follows.

$$ \varDelta \boldsymbol{CBPI}={\boldsymbol{CBPI}}^t-{\boldsymbol{CBPI}}^0=C{\mathrm{I}}^t\cdot {\mathrm{PG}}^t\cdot {\mathrm{LP}}^t\cdot {\mathrm{VI}}^t-{\mathrm{CI}}^0\cdot {\mathrm{PG}}^0\cdot {\mathrm{LP}}^0\cdot {\mathrm{VI}}^0 $$
(7)
(8)

Appendix B

Table 6 World Bank classification

Appendix C

Coal- and oil-related carbon emissions were calculated as follows:

$$ {\mathrm{CO}}_2=\sum \limits_{ij}\left({\boldsymbol{CONS}}_{ij}+{N}_{ij}+{\mathrm{CC}}_{ij}+{O}_{ij}+B\right) $$
(9)

where i represents the countries; j represents two types of energy sources (coal and oil); CONS is the total energy consumption; N is the low calorific value of energy; CC indicates the carbon content in the particular energy source; O is the carbon oxidation factor, which is assumed to be fixed at unity; and B is the molecule ratio of carbon dioxide to carbon, i.e., 44/12.

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Chen, J., Li, Z., Song, M. et al. Decomposing the global carbon balance pressure index: evidence from 77 countries. Environ Sci Pollut Res 28, 7016–7031 (2021). https://doi.org/10.1007/s11356-020-11042-1

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