The dynamics of a long-lasting effusive eruption modulated by Earth tides

Deciphering eruptive dynamics in near-real time is essential when dealing with hazard assessment and population evacuation. Recognition of specific patterns in time-series measured during volcanic activity may help decipher distinctive behavior at active volcanoes, providing insights into the underl...

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Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Dumont, Stéphanie, Le Mouël, Jean-Louis, Courtillot, Vincent, Lopes, Fernando, Sigmundsson, Freysteinn, Coppola, Diego, Eibl, Eva P. S., Bean, Christopher J.
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2020
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Online Access:https://dair.dias.ie/id/eprint/1156/
https://dair.dias.ie/id/eprint/1156/1/The%20dynamics%20of%20a%20long-lasting%20effusive%20eruption%20modulated%20by%20Earth%20tides.pdf
https://www.sciencedirect.com/science/article/abs/pii/S0012821X20300881
https://doi.org/10.1016/j.epsl.2020.116145
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Summary:Deciphering eruptive dynamics in near-real time is essential when dealing with hazard assessment and population evacuation. Recognition of specific patterns in time-series measured during volcanic activity may help decipher distinctive behavior at active volcanoes, providing insights into the underlying driving mechanisms. Multi-parameter data sets usually agree on the overall trend characterizing the temporal evolution of an eruption providing insights into the first-order eruptive dynamics. However, second-order variations detected in different data sets remain often poorly understood. The 2014-2015 Holuhraun eruption (Iceland) offers an excellent opportunity to investigate the dynamics of a long-lasting effusive eruption. We analyze the seismic tremor and the volcanic radiated power emitted by the lava field during the 6 months of the eruption using Singular Spectrum Analysis (SSA). In both geophysical time-series, we identify periods from ∼5 to ∼32 days coinciding with periods of Earth tides. Here we show that ∼50% of both signals are composed of tidal periods suggesting that magma movements follow frequencies imposed by lunisolar forces within the crust and at Earth’s surface