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InSAR Observations of Ground Deformation

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Abstract

Measurements of ground deformation have been used by geodesists to investigate natural and man-made phenomena since the 19th century. Since the early 1990s, Interferometric Synthetic Aperture Radar (InSAR) has changed the way that geodesists view the Earth, facilitating deformation monitoring in remote and inaccessible locations, and providing insight into spatially and temporally complex processes. Unsurprisingly, InSAR observations have pushed forth a new era in volcano deformation studies from both a monitoring and research perspective. InSAR observations of volcanic ground deformation enable the detection of subsurface magma, and therefore play a key role in eruptive hazard assessments. However, these observations have also shed new light on all aspects of volcanic behaviour, contributing to our understanding of the eruption cycle, hydrothermal systems and the formation of continental crust. One of the most significant achievements of volcano InSAR has been the identification and characterisation of magma inputs into the crust that would have otherwise gone unnoticed (e.g. Lu and Dzurisin 2014). Such observations of magma movement and other slow, long-term processes are crucial in determining how magmatic plumbing develops and evolves beneath a volcano (Dzurisin 2003; Cashman and Biggs 2014), but the mechanism responsible is often ambiguous.

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  1. Department of Spatial Sciences, Curtin University, Perth, Australia

    Amy Laura Parker

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Parker, A.L. (2017). Introduction. In: InSAR Observations of Ground Deformation. Springer Theses. Springer, Cham. https://doi.org/10.1007/978-3-319-39034-5_1

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