Preprints
https://doi.org/10.5194/egusphere-2026-1065
https://doi.org/10.5194/egusphere-2026-1065
07 Apr 2026
 | 07 Apr 2026
Status: this preprint is open for discussion and under review for The Cryosphere (TC).

Evolution of L-band SAR Response for Soil Freeze/Thaw Monitoring: A Case Study Over Snow-Covered Canadian Mid-latitude Agricultural Region

Zeinab Akhavan, Richard Kelly, Peter Toose, Aaron Thompson, Wei Wang, Benoit Montpetit, Alex Gélinas, and Alexandre Roy

Abstract. Soil freeze/thaw (F/T) cycles are critical regulators of global hydrological and biogeochemical processes, yet monitoring these subsurface dynamics beneath snow cover remains a significant observational challenge. There is a corresponding need for physically-based retrieval frameworks to support upcoming spaceborne Earth observation missions, such as the NASA-ISRO Synthetic Aperture Radar (NISAR) mission. Despite the importance of these cycles, there remains a critical lack of understanding regarding L-band Synthetic Aperture Radar (SAR) response beneath snow cover, primarily resulting from a reliance on coarse-resolution data and a lack of coincident, season-long ground validation. To address this, we introduce an integrated physical framework that couples high-resolution (1 m) airborne L-band (1.3 GHz) observations with coincident in situ measurements of soil temperature and permittivity. This approach utilizes analysis of backscatter responses, Freeman-Durden polarimetric decomposition, and the Improved Integral Equation Model (I2EM) to physically interpret microwave scattering and characterize subnivean F/T transitions under frozen and thawed conditions. VV-polarized backscatter exhibited the strongest sensitivity to F/T transitions, increasing during thaw and decreasing under frozen soil. Decomposition analysis revealed dominant surface scattering under frozen conditions, increased surface scattering during thaw, and enhanced volume scattering associated with melt–refreeze cycles. The I2EM simulations captured the VV and HV backscatter trends within an acceptable range across most soil stations, while significantly underestimating the HH backscatter. Overall, these results advance process-level understanding of the L-band SAR response to subnivean soil F/T transitions and demonstrate the potential of high-resolution observations for improving retrieval algorithms and calibrating forthcoming global L-band satellite missions.

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Zeinab Akhavan, Richard Kelly, Peter Toose, Aaron Thompson, Wei Wang, Benoit Montpetit, Alex Gélinas, and Alexandre Roy

Status: open (until 19 May 2026)

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Zeinab Akhavan, Richard Kelly, Peter Toose, Aaron Thompson, Wei Wang, Benoit Montpetit, Alex Gélinas, and Alexandre Roy
Zeinab Akhavan, Richard Kelly, Peter Toose, Aaron Thompson, Wei Wang, Benoit Montpetit, Alex Gélinas, and Alexandre Roy

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Short summary
Soils in cold regions freeze and thaw seasonally, affecting water flow, flooding, and carbon exchange, but these changes are hard to track beneath snow. We studied a Canadian agricultural field using high-resolution airborne radar and ground measurements through winter. Radar signals changed clearly as soils froze and thawed, with one polarization being most sensitive. Our results improve understanding of frozen soils and support future satellite monitoring.
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