Journal
SCIENCE OF THE TOTAL ENVIRONMENT
Volume 863, Issue -, Pages -Publisher
ELSEVIER
DOI: 10.1016/j.scitotenv.2022.160963
Keywords
Land use and land cover change; Carbon budget; Carbon emission; Terrestrial ecosystem; Bookkeeping model
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Scientific estimation of carbon emissions induced by historical land use and land cover change is important in improving carbon budget estimates and understanding the future carbon-sink potential. This study re-estimates China's carbon emissions for 1700-1980 using updated data and a bookkeeping model, revealing the significant changes caused by land use and cover change.
Scientific estimation of carbon emissions induced by historical land use and land cover change (LUCC) can improve the accuracy of terrestrial ecosystem carbon budget estimates and deepen understanding of the future carbon-sink poten-tial of terrestrial ecosystems. The present study, using historical-document-based data for provincial cropland, forest, and grassland area in China, and experimental-data-based information for provincial vegetation and soil organic car-bon density, re-estimates China's LUCC-induced carbon emissions for 1700-1980 using a bookkeeping model in which we updated tabulated functions for carbon losses and gains. The past 300 years have witnessed a dramatic LUCC in China. The cropland area has increased by 67.11 million ha, while the forest and grassland areas have decreased by 127.96 million ha and 16.72 million ha, respectively. Accordingly, the net carbon emissions for 1700-1980 are 6.17-12.35 Pg C, with 8.55 Pg C in the moderate scenario. Among the contributing factors, deforestation was the larg-est carbon source, accounting for over 90 % of the total carbon emissions. According to our estimates, over 70 % of carbon emissions were caused by harvesting wood, while <30 % were from converting forest and grassland to crop-land. Spatially, for the whole period, carbon emissions in southwestern China (Chuan-Yu, Yunnan, and Guangxi), northeastern China (Liaoning, Jilin, and Heilongjiang), and parts of northwestern China (Gan-Ning, Qinghai, and Xinjiang) were as high as 6.03 Pg C, accounting for 70 % of the total carbon emissions. Extending previous studies, we updated the historical LUCC data, carbon density data, and tabulated functions for carbon losses and gains. The es-timation results objectively reveal the historical spatiotemporal changes in LUCC-induced emissions.
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