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Acoustic noise and temperature monitoring of the Crater Lake of Mount Ruapehu Volcano
Authors:AW Hurst  Jean Vandemeulebrouck
Institution:aKelburn Centre, Institute of Geological and Nuclear Sciences, P.O. Box 1320, Wellington, New Zealand;bLaboratoire d'Instrumentation Géophysique, Université de Savoie, 73376 Le Bourget du Lac, France;cCentre de Recherches Volcanologiques (CNRS), Clermont-Ferrand, France
Abstract:Acoustic signals in Ruapehu Crater Lake, which are now being telemetered via a satellite transmission system, show promise as a possible precursor of increased volcanic activity from Ruapehu. The start of a recent period of rapid heating of Crater Lake was preceded by low-frequency (2 Hz) acoustic signals. These accompanied similar frequency seismic signals, but seemed to be produced independently. Audio-frequency (350–3000 Hz) acoustic noise also showed a very clear peak shortly before the lake temperature started to rise.
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