4.6 Article

Surface Soil Moisture Inversion and Distribution Based on Spatio-Temporal Fusion of MODIS and Landsat

Journal

SUSTAINABILITY
Volume 14, Issue 16, Pages -

Publisher

MDPI
DOI: 10.3390/su14169905

Keywords

soil moisture; drought index; drought; remote sensing; desert steppe

Funding

  1. special research project of the China Institute of Water Resources and Hydropower Research [MK2020J11]
  2. Inner Mongolia Applied technology research and development fund project [2021GG0020]
  3. IWHR Research & Development Support Program [MK0145B022021]
  4. major special projects and projects of the science and technology plan of the Inner Mongolia Autonomous Region [2020ZD0020, 2021GG0050]
  5. IWHR Internationally-oriented Talents Program
  6. [2021ZY0027]

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Soil moisture is important for hydrology, climate, agriculture, and ecology, and remote sensing is a crucial tool for estimating soil moisture over large areas. This study analyzed the soil moisture of different vegetation covers in Inner Mongolia and established a soil moisture inversion model using multispectral fusion bands. The results showed a strong correlation between the model and measured soil water content, indicating its effectiveness in reflecting the actual condition of surface soil moisture in different vegetation covers.
Soil moisture plays an important role in hydrology, climate, agriculture, and ecology, and remote sensing is one of the most important tools for estimating the soil moisture over large areas. Soil moisture, which is calculated by remote sensing inversion, is affected by the uneven distribution of vegetation and therefore the results cannot accurately reflect the spatial distribution of the soil moisture in the study area. This study analyzes the soil moisture of different vegetation covers in the Wushen Banner of Inner Mongolia, recorded in 2016, and using Landsat and MODIS images fused with multispectral bands. Firstly, we compared and analyzed the ability of the visible optical and short-wave infrared drought index (VSDI), the normalized differential infrared index (NDII), and the short-wave infrared water stress index (SIWSI) in monitoring the soil moisture in different vegetation cover soils. Secondly, we used the stepwise multiple regression analysis method in order to correlate the multispectral fusion bands with the field-measured soil water content and established a soil moisture inversion model based on the multispectral fusion bands. As the results show, there was a strong correlation between the established model and the measured soil water content of the different vegetation cover soils: in the bare soil, R2 was 0.86; in the partially vegetated cover soil, R2 was 0.84; and in the highly vegetated cover soil, R2 was 0.87. This shows that the established model could better reflect the actual condition of the surface soil moisture in the different vegetation covers.

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