Abstract

<strong class="journal-contentHeaderColor">Abstract.</strong> The small-aperture Spitsbergen seismic array (SPITS) has been in continuous operation at Janssonhaugen for decades. The high-Arctic location in the Svalbard archipelago makes SPITS an ideal laboratory for the study of cryoseisms, a nontectonic class of seismic events caused by freeze processes in ice, ice–soil, and ice–rock materials. We extracted a catalog of <span class="inline-formula">&gt;</span> 100 000 events from the nearly continuous observation period between 2004 and 2021, characterized by short-duration ground shaking of just a few seconds. This catalog contains two main subclasses where one subclass is related to underground coal-mining activities and the other is inferred to be dominated by frost quakes resulting from thermal-contraction cracking of ice wedges and crack-filling vein ice. This inference is supported by the correspondence between peaks in observed seismicity with peaks in modeled ground thermal stress, based on a Maxwellian thermo-viscoelastic model constrained by borehole observations of ground temperature. The inferred frost quakes appear to be dominated by surface wave energy and SPITS proximal source positions, with three main areas that are associated with dynamic geomorphological features, i.e., erosional scarps and a frozen-debris/solifluction lobe. Seismic stations providing year-round, high-temporal-resolution measurements of ground motion may be highly complementary to satellite remote sensing methods, such as InSAR (interferometric synthetic aperture radar), for studying the dynamics of periglacial environments. The long-term observational record presented in this study, containing tens of thousands of cryoseismic events, in combination with a detailed record of borehole ground temperature observations, provides a unique insight into the spatiotemporal patterns of cryoseisms. The observed patterns may guide the development of models that can be used to understand future changes to cryoseismicity based on projected temperatures.

Highlights

  • 25 Cryoseisms are a nontectonic class of seismic events caused by freeze processes in ice, ice-soil and ice-rock materials (Lacroix, 1980)

  • In order to improve the precision of the source localisation by coherent Matched-field processing (MFP), only events recorded by at least five seismometers 280 were located for a total of 137,456 located short duration events

  • 5 Conclusion We studied the spatial and temporal patterns of the class of seismicity that lead to short duration ground shaking at the Spitsbergen seismic array (SPITS) 410 array in Adventdalen, based on a catalogue of >100 000 events recorded between 2004 and 2021

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Summary

Introduction

25 Cryoseisms are a nontectonic class of seismic events caused by freeze processes in ice, ice-soil and ice-rock materials (Lacroix, 1980). The buildup of thermal stress in frozen soils during intense periods of cooling can lead to tensional fracturing and explosive pressure release (Barosh, 2000; Battaglia et al, 2016). Since this pressure release triggers the propagation of seismic waves, these events are sometimes referred to as frost quakes (e.g. Okkonen et al, 2020).

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