Abstract

This paper provides a review of the progress in regard to the InSAR remote sensing technique and its applications in earth and environmental sciences, especially in the past decade. Basic principles, factors, limits, InSAR sensors, available software packages for the generation of InSAR interferograms were summarized to support future applications. Emphasis was placed on the applications of InSAR in seismology, volcanology, land subsidence/uplift, landslide, glaciology, hydrology, and forestry sciences. It ends with a discussion of future research directions.

Highlights

  • Interferometric synthetic aperture radar (InSAR) is a rapidly evolving remote sensing technology that directly measures the phase change between two phase measurements of the same ground pixel of Sensors 2009, 9 the Earth’s surface

  • The present review summarizes the most recent developments of InSAR remote sensing technology and its broad applications in earth and environmental systems, especially in the past decade

  • InSAR is a remote sensing technique using two or more SAR phase images acquired at different times to generate maps to detect and map changes of spatial and/or dielectric properties of the ground surface by using differences in the phase of the waves returning to the satellite or aircraft [1,3,4,6,13]

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Summary

Introduction

Interferometric synthetic aperture radar (InSAR) is a rapidly evolving remote sensing technology that directly measures the phase change between two phase measurements of the same ground pixel of Sensors 2009, 9 the Earth’s surface. Any factor that can affect the phase of the backscattered radar signal can affect the fringe pattern and the number of fringes in the interferogram, and can potentially be measured by the InSAR technology. These measurements include surface displacements, land topography, land changes, land subsidence/uplift, water levels, soil moisture, snow accumulation, stem volume of forest, etc. The present review summarizes the most recent developments of InSAR remote sensing technology and its broad applications in earth and environmental systems, especially in the past decade. InSAR applications in seismology, volcanology, land subsidence/lift, landslide, glaciology, hydrology, and forestry, respectively

Phase Change–Basic Measurement of InSAR
Factors That Impact the Phase of an Image Pixel
InSAR and Interferogram
Range Change Detection from Interferogram
Selection of Interferometric Pair
Formation of an Interferogram
Limits of Conventional InSAR and New Remedy
SAR Sensors for InSAR and InSAR Software
Applications of InSAR
Application in Seismology
Application of InSAR in Volcanology
Land Subsidence and Uplift
Landslides
Applications of InSAR in Glaciology
Soil Moisture Monitoring
Water Level Measurement and Monitoring
Applications in Forestry
Discussion and Outlook
39. The Stationary Office
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