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A 1000-year history of cropland cover change along the middle and lower reaches of the Yellow River in China

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Abstract

Landscape in the middle and lower reaches of the Yellow River in China has undergone significant changes for thousands of years due to agricultural expansion. Lack of reliable long-term and high-resolution historical cropland data has limited our ability in understanding and quantifying human impacts on regional climate change, carbon and water cycles. In this study, we used a data-driven modeling framework that combined multiple sources of data (historical provincial cropland area, historical coastlines, and satellite data-based maximum cropland extent) with a new gridding allocation model for croplands distribution to reconstruct a historical cropland dataset for the middle and lower reaches of the Yellow River at a 10-km resolution for 58 time points ranging from the period 1000 to 1999. The cropland area in the study area increased by 2.3 times from 21.87 million ha in 1000 to 50.64 million ha in 1999. Before 1393, the area of cropland increased slowly and was primarily concentrated in the Weihe and Fenhe plains. From 1393–1820, the area of cropland increased rapidly, particularly on the North China Plain. Since 1820, cropland cover has tended to become saturated. Our newly reconstructed results agreed well with remotely sensed data as well as historical document-based facts regarding cropland distribution.

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Correspondence to Fanneng He.

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Foundation: National Natural Science Foundation of China, No.42201263; National Key Research and Development Program of China on Global Change, No.2017YFA0603304

Author: Yang Fan (1991–), PhD and Associate Professor, specialized in long-term land use/cover change and their environmental effects.

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Yang, F., Zhang, H., He, F. et al. A 1000-year history of cropland cover change along the middle and lower reaches of the Yellow River in China. J. Geogr. Sci. 34, 921–941 (2024). https://doi.org/10.1007/s11442-024-2233-z

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  • DOI: https://doi.org/10.1007/s11442-024-2233-z

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