Abstract

Generally, the characterization of land surface roughness is obtained from the analysis of height variations observed along transects (e.g., root mean square (RMS) height, correlation length, and autocorrelation function). These surface roughness measurements are then used as inputs for surface dynamics modeling, e.g., for soil erosion modeling, runoff estimation, and microwave remote sensing scattering modeling and calibration. In the past, researchers have suggested various methods for estimating roughness parameters based on ground measurements, e.g., using a pin profilometer, but these methods require physical contact with the land and can be time-consuming to conduct. The target of this research is to develop a technique for deriving surface roughness characteristics from digital camera images by applying photogrammetric and geographical information systems (GIS) analysis techniques. First, ground photos acquired by a digital camera in the field were used to create a point cloud and 3D digital terrain model (DTM). Then, the DTM was imported to a GIS environment to calculate the surface roughness parameter for each field site. The results of the roughness derivation can be integrated with soil moisture for backscattering simulation, e.g., for inversion modeling to retrieve the backscattering coefficient. The results show that the proposed method has a high potential for retrieving surface roughness parameters in a time- and cost-efficient manner. The selection of homogeneous fields and the increased spatial distribution of sites in the study area will show a better result for microwave backscattering modeling.

Highlights

  • Surface roughness plays a key role in microwave remote sensing backscattering and modeling and is an important parameter for studies on soil moisture, soil erosion, and hydrological processes

  • We proposed a simple approach for the measurement of land surface roughness using a hand-held digital camera and photogrammetry techniques

  • Researchers have tried to use the inverse model for backscattering without parametrizing the surface roughness, this method requires soil moisture measurement in situ and is often not applicable in the forward model because of the lack of in situ soil moisture data, and because it is very costly to set up the soil moisture measurement network

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Summary

Introduction

Surface roughness plays a key role in microwave remote sensing backscattering and modeling and is an important parameter for studies on soil moisture, soil erosion, and hydrological processes. Microwave remote sensing images are commonly used for large-area soil moisture retrieval and mapping from space, but despite much research, accurate soil moisture estimation is still challenging due to the inherent dependency of the backscattered microwave radiation on both the geometric and dielectric properties of the land surface [1,2,3,4,5]. In recent years some methods have been developed for inverting both soil moisture and soil surface roughness separately using multi-temporal synthetic aperture radar (SAR) images and/or multi-frequency, multi-polarized SAR data, their performance has mainly been evaluated at relatively small scales, and their suitability for large-area operational usage is uncertain [10,11,12]

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