Evaluation of integrating topographic wetness index with backscattering coefficient of TerraSAR-X image for soil moisture estimation in a mountainous region. (February 2016)

• Record Type: Journal Article
• Authors: Lei, Shaogang; Chen, Hequn; Bian, Zhengfu; Liu, Zhenguo
• Is Part Of: Ecological indicators. Volume 61:Part 2(2016)
• Page Start: 624
• Page End: 633
• Publication Date: 2016-02
• Subjects: Soil water content -- TerraSAR-X -- Topographic wetness index -- Backscattering coefficient; Environmental monitoring -- Periodicals; Environmental management -- Periodicals; Environmental impact analysis -- Periodicals; Environmental risk assessment -- Periodicals; Sustainable development -- Periodicals; 333.71405
• DOI: 10.1016/j.ecolind.2015.10.013
• Languages: English
• ISSNs: 1470-160X

Abstract

Highlights: Mountainous terrain can disturb the empirical moisture estimation models. Integration of TWI into model can improve the estimation in mountainous region. The most reasonable penetration depth of the microwave X-band is verified at 5 cm. Abstract: The estimation of soil moisture by using the backscattering coefficient of radar in a mountainous region is a challenging task due to the complex topography, which impacts the distribution of soil moisture and changes the backscattering coefficient. Complicated terrain can disturb empirical moisture estimation models, thereby, the resulting estimates of soil moisture are very unlikely reliable. This article proposed an innovative way of integration of the topographic wetness index (TWI) and the backscattering coefficient of soil obtained from the TerraSAR-X image, which improves the accuracy of measurement of the soil moisture. The standard estimation error and the coefficient of determination from the model were used to evaluate the performance of TWI. Our results show that the standard estimation error was decreased from: (1) 4.0% to 3.3% cm 3 cm −3 at a depth of 5 cm and (2) 4.5% to 3.9% cm 3 cm −3 at a depth of 10 cm. The most reliable estimation was observed at a depth of 5 cm, when it was compared with those of 0–5 cm, 10 cm and 15 cm. The TWI from the digital elevation model (DEM) is useful as a constraint condition for modeling work. This article concludes that the integration of the backscattering coefficient of soil with TWI can significantly reduce the uncertainty in the estimation of soil moisture in a mountainous region.