Forecasting and Planning for Volcanic Hazards, Risks, and Disasters 2021
DOI: 10.1016/b978-0-12-818082-2.00003-2
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Volcano geodesy: A critical tool for assessing the state of volcanoes and their potential for hazardous eruptive activity

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Cited by 6 publications
(2 citation statements)
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“…This flat summit is likely the result of interpolation over gaps created by shadow and signal overlay areas in the TSX data used. When georeferencing, this discrepancy causes the deformation signal to appear stretched and greatest on the eastern edge of the crater floor (Figure 5c), similar to the deformation signal shown in Poland et al (2020) and Poland and de Zeeuw-van Dalfsen (2021). In reality, the deformation signal is greatest in the center of the crater floor and is bounded to the west by the crater walls (Figure 5d).…”
Section: Influence Of Dem Accuracymentioning
confidence: 77%
“…This flat summit is likely the result of interpolation over gaps created by shadow and signal overlay areas in the TSX data used. When georeferencing, this discrepancy causes the deformation signal to appear stretched and greatest on the eastern edge of the crater floor (Figure 5c), similar to the deformation signal shown in Poland et al (2020) and Poland and de Zeeuw-van Dalfsen (2021). In reality, the deformation signal is greatest in the center of the crater floor and is bounded to the west by the crater walls (Figure 5d).…”
Section: Influence Of Dem Accuracymentioning
confidence: 77%
“…Natural processes such as volcanic activity produce surface displacements due to many phenomena, including magma recharge/deployment and migration, fluid flow, and other internal processes related to magma crystallization and degassing. Volcano geodesy is crucial to define the state of volcanoes (Poland and de Zeeuw-van Dalfsen, 2021) and for eruptive hazard assessment (Sparks et al, 2012;Biggs et al, 2014). The accurate measurement of surface deformation is one of the most relevant parameters to estimate tectonic stress accumulation and release (DeMets et al, 1990) for studying the seismic cycle (Wright et al, 2004;Weston et al, 2011) and the intraplate coupling (Hashimoto et al, 2009).…”
Section: Introductionmentioning
confidence: 99%