Estimating high-resolution soil moisture by combining data from a sparse network of soil moisture sensors and remotely sensed MODIS LST information

被引:0
作者
Gemitzi, Alexandra [1 ]
Kofidou, Maria [1 ]
Falalakis, George [2 ]
Fang, Bin [3 ]
Lakshmi, Venkat [3 ]
机构
[1] Democritus Univ Thrace, Fac Engn, Dept Environm Engn, V Sofias 12, Xanthi 67100, Greece
[2] Kosmio 1302, Komotini 69100, Greece
[3] Dept Civil & Environm Engn, Olsson Hall 102E,151 Engineers Way, Charlottesville, VA 22904 USA
来源
HYDROLOGY RESEARCH | 2024年 / 55卷 / 09期
关键词
in situ soil moisture monitoring; MODIS LST; soil moisture; soil moisture downscaling; SURFACE-TEMPERATURE;
D O I
10.2166/nh.2024.043
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The present work demonstrates a methodology for acquiring high-resolution soil moisture information, namely at 1 km at a daily time step, utilizing data from a sparse network of soil moisture sensors and remotely sensed Land Surface Temperature (LST). Building on previous research and highlighting the strong correlation between surface soil moisture and LST, as a result of the thermal inertia, we first, evaluated the correlation between Moderate Resolution Imaging Spectroradiometer (MODIS) LST and ground-based soil moisture information from soil moisture sensors installed in a pilot area in Northeastern Greece, namely the Komotini test site, from October 2021. Second, a regression formula was developed for three out of six soil moisture sensors, keeping the three remaining monitoring stations serving as a validation set. Furthermore, regression coefficients were interpolated at 1 km and the regression equations were applied for the entire study area, thus acquiring soil moisture information at a spatial resolution of 1 km at the daily time step. The verification process indicated a reasonable accuracy, with a mean absolute error (MAE) of <0.02 m(3)/m(3). The results were considerably better than using a simple interpolation or downscaled daily 1-km SMAP soil moisture.
引用
收藏
页码:905 / 920
页数:16
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