Abstract:Accurate monitoring of soil water content (SWC) is essential for evaluating crop water status and optimizing agricultural water management. Conventional thermal infrared remote sensing often neglects the temporal lag between canopy and air temperature responses, potentially introducing estimation bias. The canopy-air temperature time-lag effect was integrated into UAV-based thermal infrared remote sensing for improved SWC estimation. A two-year winter wheat experiment with four irrigation levels was conducted, using fixed infrared sensors (SI-411) and UAV thermal imagery. The peak-time difference method quantified the lag and its response to soil moisture gradients. Four time-lag-adjusted SWC models were developed, i.e., theoretical, empirical, hybrid and canopy-air temperature difference models. Results showed that lag times in W1~W3 treatments did not differ significantly, while W4 (low moisture) had shorter lags. Lag time decreased markedly when SWC fell below 50%~65% of field capacity. Introducing the lag effect reduced the mean crop water stress index (CWSI) by 0.05~0.13, with hybrid model producing the most physiologically consistent spatial patterns. Except for the theoretical model, R2 were improved, with the empirical CWSI model performing best (2022: R2=0.53, RMSE was 1.99%;2023: R2=0.51, RMSE was 2.13%). The findings can underscore the importance of thermal response dynamics for enhancing SWC estimation and provide methodological advances for large-scale UAV-based agricultural water stress monitoring.