Seasonally soil freeze-thaw process has a profound impact on hydrologic cycle, meteorology and soil erosion. A
useful indicator to evaluate the soil freeze-thaw intensity is the amount of phase transition water content (PTWC) in soil
pores. In this research, a large dataset of simulated brightness temperature were generated using Advanced Integral
Equation Model (AIEM) based on the configuration of the Advanced Microwave Scanning Radiometer for the Earth
Observing System (AMSR-E) with soil parameters changing in a wide range. Through analyzing of the simulated
brightness temperature and PTWC, a nearly linear correlation relationship existed between the brightness temperature
difference of frozen and thawed soil in vertical or horizontal polarization to the PTWC, but it was affected by soil
roughness. Then a statistical algorithm was put forward to estimate the PTWC using a combined brightness temperature
of vertical and horizontal polarization. Finally, this algorithm was applied to the ground-based radiometer observation
and validated by the ground truth. The results showed that this algorithm had an acceptable precision with a root mean
square error (RMSE) of 0.0261 (m3/m3) and the absolute error less than 0.02 (m3/m3) was about 82.67%. The advantage
of this algorithm is that it combines v and h polarization brightness temperature through adding different weights on
them so as to weaken the influence of surface roughness and achieves the desired results.
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