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Fig. 1 | Journal of Applied Volcanology

Fig. 1

From: Using infrasound to constrain ash plume rise

Fig. 1

Infrasound signals and velocity profiles. The recorded infrasound signals, de-trended and high-pass filtered (0.1 Hz) for removal of very long-period noise/drift (a, c), and calculated mass velocity profiles (b, d) for event 2 (a, b), and event 17 (c, d)

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