FN Archimer Export Format PT J TI Tide-induced microseismicity in the Mertz glacier grounding area, East Antarctica BT AF BARRUOL, Guilhem CORDIER, Emmanuel BASCOU, Jerome FONTAINE, Fabrice R. LEGRESY, Benoit LESCARMONTIER, Lydie AS 1:1;2:1;3:2;4:1;5:3;6:3,4; FF 1:;2:;3:;4:;5:;6:; C1 Univ Paris Diderot, CNRS UMR 7154, Sorbonne Paris Cite, Lab GeoSci Reunion,Univ La Reunion,Inst Phys Glob, FR-97744 St Denis, France. Univ St Etienne, CNRS UMR 6524, Univ Lyon, Lab Magmas & Volcans, St Etienne, France. Lab Etud Geophys & Oceanog Spatiale, Toulouse, France. Australian Natl Univ, Res Sch Earth Sci, Acton, ACT, Australia. C2 UNIV PARIS 07, FRANCE UNIV ST ETIENNE, FRANCE LEGOS, FRANCE UNIV AUSTRALIAN NATL, AUSTRALIA IF 4.456 TC 23 UR https://archimer.ifremer.fr/doc/00244/35567/34098.pdf LA English DT Article CR NIVMER 08-DDU VT 93 / NIVMER08 BO L'Astrolabe Marion Dufresne DE ;icequakes;Mertz glacier;tide;Antarctica;cryoseismology;Adélie land AB The deployment of a seismic network along the Adelie and George V coasts in East Antarctica during the period 2009-2012 provides the opportunity to monitor cryoseismic activity and to obtain new insights on the relationship between tidal cycles and coastal glacier dynamics. Here we focus on records from a seismometer located on a rocky outcrop in the vicinity of the grounding line of the 35 km broad Mertz glacier, a major outflow of this region. We detect numerous icequakes (50,000 events within 10 months and up to 100 events/h) and demonstrate their clear tidal modulation. We suggest that they result from ice friction and fracturing around the rocky peak and from the glacier flexure in response to the falling and rising tides at its grounding area. We propose that such icequake monitoring could be used as a climate proxy since grounding lines are subject to migrate with sea level changes. PY 2013 PD OCT SO Geophysical Research Letters SN 0094-8276 PU Amer Geophysical Union VL 40 IS 20 UT 000330514200015 BP 5412 EP 5416 DI 10.1002/2013GL057814 ID 35567 ER EF