Mapping high-resolution soil moisture and properties using distributed temperature sensing data and an adaptive particle batch smoother

Journal Article (2016)
Author(s)

Jianzhi Dong (TU Delft - Water Resources)

Susan Steele-Dunne (TU Delft - Water Resources)

Tyson E. Ochsner (Oklahoma State University)

Christine E. Hatch (University of Massachusetts Amherst)

Chadi Sayde (Oregon State University)

J.S. Selker (Oregon State University, TU Delft - Water Resources)

Scott Tyler (University of Nevada, Reno)

Michael H. Cosh (USDA-ARS Hydrology and Remote Sensing Laboratory)

NC van de Giesen (TU Delft - Water Resources)

Research Group
Water Resources
Copyright
© 2016 J. Dong, S.C. Steele-Dunne, Tyson E. Ochsner, Christine E. Hatch, Chadi Sayde, J.S. Selker, Scott Tyler, Michael H. Cosh, N.C. van de Giesen
DOI related publication
https://doi.org/10.1002/2016WR019031
More Info
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Publication Year
2016
Language
English
Copyright
© 2016 J. Dong, S.C. Steele-Dunne, Tyson E. Ochsner, Christine E. Hatch, Chadi Sayde, J.S. Selker, Scott Tyler, Michael H. Cosh, N.C. van de Giesen
Research Group
Water Resources
Issue number
10
Volume number
52
Pages (from-to)
7690-7710
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Abstract

This study demonstrated a new method for mapping high-resolution (spatial: 1 m, and temporal: 1 h) soil moisture by assimilating distributed temperature sensing (DTS) observed soil temperatures at intermediate scales. In order to provide robust soil moisture and property estimates, we first proposed an adaptive particle batch smoother algorithm (APBS). In the APBS, a tuning factor, which can avoid severe particle weight degeneration, is automatically determined by maximizing the reliability of the soil temperature estimates of each batch window. A multiple truth synthetic test was used to demonstrate the APBS can robustly estimate soil moisture and properties using observed soil temperatures at two shallow depths. The APBS algorithm was then applied to DTS data along a 71 m transect, yielding an hourly soil moisture map with meter resolution. Results show the APBS can draw the prior guessed soil hydraulic and thermal properties significantly closer to the field measured reference values. The improved soil properties in turn remove the soil moisture biases between the prior guessed and reference soil moisture, which was particularly noticeable at depth above 20 cm. This high-resolution soil moisture map demonstrates the potential of characterizing soil moisture temporal and spatial variability and reflects patterns consistent with previous studies conducted using intensive point scale soil moisture samples. The intermediate scale high spatial resolution soil moisture information derived from the DTS may facilitate remote sensing soil moisture product calibration and validation. In addition, the APBS algorithm proposed in this study would also be applicable to general hydrological data assimilation problems for robust model state and parameter estimation.

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