Analyzing the tremor of the Holuhraun eruption 2014-2015 using tremor modelling

<p>The 2014-2015 Holuhraun eruption was the largest eruption in Iceland in the last 230 years. After magma ascended below <!-- Gibt es ein Paper das belegt, dass Magmaaufstieg den Dike getriggert hat? Ich denke, das ist eher Spekulation. Vllt. wäre es besser einfach zu sagen, „From ice-covered Bardarbunga an about 2 week long EQ migration …“ -->the Bárðarbunga volcano’s icecap, an about 2 week long lateral migration of earthquakes was observed; later interpreted as dike formation in 4km to 6km depth<!-- Noch die Tiefe (formation [in 4-6km depth]) mit reinbringen? --><!-- Ja kannst du machen. -->. An eruption started on 29<sup>th</sup> and 31<sup>st</sup> of August 2014 at Holuhraun. During dike formation and eruption a long-lasting seismic signal called tremor was recorded by seismometers in the area. Eruptive tremor emerged with the onset of the eruptions on 29<sup>th</sup> and 31<sup>st</sup> of August . Tremor sources were located and interpreted in the context of the fissure and the lava flow field. However, a complete geophysical model to explain these is missing. Our starting point is the model on tremor generation based on conduit wall vibrations exited by laminar flow<!-- Bitte anpassen. --> (B. Julian 1994) to replicate the observed tremor signals. We performed a grid search and compare it with other models. In the range of rock parameter tolerance, we present implied characteristics of frequency and amplitude of the signals, if the Julian model were used as explanation for the tremor signals.</p>