
A groundbreaking study has introduced a new method for monitoring soil freeze-thaw (FT) cycles from space, offering improved accuracy in tracking environmental changes critical to climate modeling, agriculture, and hydrology. Researchers from Fudan University, the University of Twente, and Chengdu University of Information Technology have developed an enhanced algorithm that leverages L-band microwave data from NASA’s SMAP satellite to map soil FT processes with unprecedented precision. The findings, published on 10 September 2025 in the Journal of Remote Sensing, demonstrate significant advancements in capturing regional and diurnal variations in soil conditions.
Soil FT transitions influence surface albedo, moisture, and heat fluxes, impacting weather patterns and hydrological cycles. Traditional large-scale models often overlook diurnal temperature fluctuations and surface heterogeneity, limiting their accuracy. The new dynamic parameter optimization algorithm, an improvement on the existing Diurnal Amplitude Variation–based Freeze–Thaw (DAV-FT) model, addresses these challenges by incorporating three adaptive parameters: detection period, variance window, and threshold sensitivity. These parameters are optimized regionally to account for diverse land cover, terrain, and climate conditions, enabling more accurate differentiation of frozen and thawed soil states based on L-band brightness temperature data.

The study’s results highlight a substantial improvement in performance, with the optimized algorithm achieving an overall classification accuracy (OA) above 70% across 89.36% of tested regions, compared to 54.43% for the original model. Notable success was observed in areas like the Qinghai–Tibet Plateau, southwestern Eurasia, and southern North America. Validation against 828 in situ soil temperature stations confirmed a median accuracy of 92%, surpassing both fixed-parameter models and existing SMAP FT products. The algorithm also showed strong alignment with ERA5-Land (81.28%) and SMAP-FT (79.54%) datasets, underscoring its reliability.
The enhanced DAV-FT algorithm excels in capturing subtle FT transitions, particularly in high-latitude and mountainous regions where previous methods struggled. By accounting for diurnal temperature cycles and regional variability, it provides a robust tool for continuous monitoring of soil states. This advancement supports better assessment of permafrost dynamics, water availability, and land-atmosphere energy exchanges, which are vital for understanding climate change impacts and refining global land-surface models.
Funded by the National Key R&D Program of China, the Inner Mongolia Autonomous Region’s Key Research Program, the Yan Liyuan–ENSKY Foundation, and the National Natural Science Foundation of China, this research marks a significant step toward high-resolution, global-scale environmental monitoring. The algorithm’s adaptability makes it a valuable asset for climate scientists, agricultural planners, and hydrologists seeking to address the challenges of a changing planet.
About Journal of Remote Sensing
The Journal of Remote Sensing, an online-only Open Access journal published in association with AIR-CAS, promotes the theory, science, and technology of remote sensing, as well as interdisciplinary research within earth and information science.

