Spatio-temporal Monitoring of Agricultural Drought in China Based on Downscaled Soil Moisture Data

Abstract. Agricultural drought threatens China's food and ecological security, and accurate spatio-temporal monitoring is key for disaster mitigation. Soil moisture is critical for drought assessment, but the accuracy of existing remote sensing-based SM products in China remains to be improved. This study develops a framework that synergistically integrates a spatiotemporally adaptive gap-filling algorithm with a machine learning-based downscaling approach, generating a seamless 0.05° monthly SM dataset for China from 2003 to 2023. The methodology harnesses the complementary strengths of random forest modeling and spatiotemporal reconstruction techniques to effectively fuse multi-source satellite observations, achieving dual improvements in SM data accuracy and spatial coverage. Using this dataset, the standardized soil moisture index was applied to characterize the spatio-temporal evolution of agricultural drought. Results demonstrate that (1) The downscaled SM dataset achieves significant improvements in both spatial resolution and accuracy, showing a 2.3–34.4 % reduction in ubRMSE and 1.2–52.7 % improvement in correlation coefficients compared to benchmark datasets. (2) Drought characterization based on the downscaled SM dataset and SSI accurately identified the extent of agricultural drought, showing a significant spatiotemporal consistency with agricultural disaster area. (3) Agricultural drought intensified significantly across China during the study period, characterized by northward migration of drought center and spatially heterogeneous aridification patterns – decreasing severity from northwest to southeast while increasing from northeast to southwest. High-frequency drought zones were predominantly clustered in ecologically vulnerable regions, particularly the agro-pastoral ecotone of northern China. (4) Distinct intra-annual drought dynamics emerged, with a southwest-to-northeast expansion dominating from January to June, followed by bidirectional propagation from the Yellow River-Huaihe River Basin (YRB-HRB) to northwestern and southeastern regions from June to December. This study provides high-accuracy data support for agricultural drought monitoring and offers scientific insights for developing regional differentiated drought mitigation strategies, which are of great significance for ensuring national food security.