A quest for unrest in multiparameter observations at Whakaari/White Island volcano, New Zealand 2007–2018

• Published in: Earth, Planets and Space
• Main Authors: Caudron C., Girona T., Jolly A., Christenson B., Savage M. K., Carniel R., Lecocq T., Kennedy B., Lokmer I., Yates A., Hamling I., Park I., Kilgour G., Mazot A.
• Other Authors: Caudron, C., Girona, T., Jolly, A., Christenson, B., Savage, M. K., Carniel, R., Lecocq, T., Kennedy, B., Lokmer, I., Yates, A., Hamling, I., Park, I., Kilgour, G., Mazot, A.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2021
• Subjects: Monitoring; Phreatic eruption; Seismic noise; Tremor; Volcanology; New Zealand; White Island
• Online Access: http://hdl.handle.net/11390/1214026; https://doi.org/10.1186/s40623-021-01506-0

The Whakaari/White Island volcano, located ~ 50 km off the east coast of the North Island in New Zealand, has experienced sequences of quiescence, unrest, magmatic and phreatic eruptions over the last decades. For the last 15 years, seismic data have been continuously archived providing potential insight into this frequently active volcano. Here we take advantage of this unusually long time series to retrospectively process the seismic data using ambient noise and tremor-based methodologies. We investigate the time (RSAM) and frequency (Power Spectral Density) evolution of the volcanic tremor, then estimate the changes in the shallow subsurface using the Displacement Seismic Amplitude Ratio (DSAR), relative seismic velocity (dv/v) and decorrelation, and the Luni-Seismic Correlation (LSC). By combining our new set of observations with the long-term evolution of earthquakes, deformation, visual observations and geochemistry, we review the activity of Whakaari/White Island between 2007 and the end of 2018. Our analysis reveals the existence of distinct patterns related to the volcano activity with periods of calm followed by cycles of pressurization and eruptions. We finally put these results in the wider context of forecasting phreatic eruptions using continuous seismic records. [Figure not available: see fulltext.].