Articles | Volume 15, issue 10
https://doi.org/10.5194/tc-15-5007-2021
https://doi.org/10.5194/tc-15-5007-2021
Research article
 | 
29 Oct 2021
Research article |  | 29 Oct 2021

Wind-induced seismic noise at the Princess Elisabeth Antarctica Station

Baptiste Frankinet, Thomas Lecocq, and Thierry Camelbeeck

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Cited articles

Barruol, G., Cordier, E., Bascou, J., Fontaine, F. R., Legrésy, B., and Lescarmontier, L.: Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica: Mertz Glacier Tide-Modulated Icequakes, Geophys. Res. Lett., 40, 5412–5416, https://doi.org/10.1002/2013GL057814, 2013. 
Belspo.: Construction and operation of the new Belgian Research Station, Dronning Maud Land, Antarctica: Final Comprehensive Environmental Evaluation Report (CEE), 135, Belgium, March 2007. 
Beyreuther, M., Barsch, R., Krischer, L., Megies, T., Behr, Y., and Wassermann, J.: ObsPy: A Python Toolbox for Seismology, Seismol. Res. Lett., 81, 530–533, https://doi.org/10.1785/gssrl.81.3.530, 2010. 
Bormann, P. and Wielandt, E.: Seismic Signals and Noise, New Manual of Seismological Observatory Practice 2, Potsdam, Deutsches GeoForschungszentrum GFZ; IASPEI, (NMSOP2), 62, 2013. 
Callens, D., Thonnard, N., Lenaerts, J. T. M., Van Wessem, J. M., Van de Berg, W. J., Matsuoka, K., and Pattyn, F.: Mass balance of the Sør Rondane glacial system, East Antarctica, Ann. Glaciol., 56, 63–69, https://doi.org/10.3189/2015AoG70A010, 2015. 
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Short summary
Icequakes are the result of processes occurring within the ice mass or between the ice and its environment. Having a complete catalogue of those icequakes provides a unique view on the ice dynamics. But the instruments recording these events are polluted by different noise sources such as the wind. Using the data from multiple instruments, we found how the wind noise affects the icequake monitoring at the Princess Elisabeth Station in Antarctica.
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