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- W2152629560 abstract "High-melt areas of glaciers and ice sheets foster a rich spectrum of ambient seismicity. These signals not only shed light on source mechanisms (e.g. englacial fracturing, water flow, iceberg detachment, basal motion) but also carry information about seismic wave propagation within glacier ice. Here, we present two approaches to measure and potentially monitor phase velocities of high-frequency seismic waves (≥1 Hz) using naturally occurring glacier seismicity. These two approaches were developed for data recorded by on-ice seasonal seismic networks on the Greenland Ice Sheet and a Swiss Alpine glacier. The Greenland data set consists of continuous seismograms, dominated by long-term tremor-like signals of englacial water flow, whereas the Alpine data were collected in triggered mode producing 1–2 s long records that include fracture events within the ice (‘icequakes’). We use a matched-field processing technique to retrieve frequency-dependent phase velocity measurements for the Greenland data. In principle, this phase dispersion relationship can be inverted for ice sheet thickness and bed properties. For these Greenland data, inversion of the dispersion curve yields a bedrock depth of 541 m, which may be too small by as much as 35 per cent. We suggest that the discrepancy is due to lateral changes in ice sheet depth and bed properties beneath the network, which may cause unaccounted mixing of surface wave modes in the dispersion curve. The Swiss Alpine icequake records, on the other hand, allow for reconstruction of the impulse response between two seismometers. The direct and scattered wave fields from the vast numbers of icequake records (tens of thousands per month) can be used to measure small changes in englacial velocities and thus monitor structural changes within the ice." @default.
- W2152629560 created "2016-06-24" @default.
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- W2152629560 date "2015-04-15" @default.
- W2152629560 modified "2023-09-25" @default.
- W2152629560 title "Using glacier seismicity for phase velocity measurements and Green's function retrieval" @default.
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- W2152629560 cites W1585031452 @default.
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- W2152629560 cites W1634644109 @default.
- W2152629560 cites W1641136069 @default.
- W2152629560 cites W1827931359 @default.
- W2152629560 cites W1837963769 @default.
- W2152629560 cites W1862851990 @default.
- W2152629560 cites W1893521577 @default.
- W2152629560 cites W1963654021 @default.
- W2152629560 cites W1964195730 @default.
- W2152629560 cites W1966749872 @default.
- W2152629560 cites W1967672975 @default.
- W2152629560 cites W1969227012 @default.
- W2152629560 cites W1969804623 @default.
- W2152629560 cites W1970508535 @default.
- W2152629560 cites W1971022140 @default.
- W2152629560 cites W1976043511 @default.
- W2152629560 cites W1977467923 @default.
- W2152629560 cites W1981770481 @default.
- W2152629560 cites W1981798449 @default.
- W2152629560 cites W1988201156 @default.
- W2152629560 cites W1992512332 @default.
- W2152629560 cites W1998242458 @default.
- W2152629560 cites W2000363768 @default.
- W2152629560 cites W2001975904 @default.
- W2152629560 cites W2003649102 @default.
- W2152629560 cites W2014459176 @default.
- W2152629560 cites W2018254568 @default.
- W2152629560 cites W2018316543 @default.
- W2152629560 cites W2021217022 @default.
- W2152629560 cites W2021322498 @default.
- W2152629560 cites W2027329183 @default.
- W2152629560 cites W2030671486 @default.
- W2152629560 cites W2030833344 @default.
- W2152629560 cites W2036221985 @default.
- W2152629560 cites W2047695905 @default.
- W2152629560 cites W2051646067 @default.
- W2152629560 cites W2051673701 @default.
- W2152629560 cites W2057516589 @default.
- W2152629560 cites W2060574279 @default.
- W2152629560 cites W2065051840 @default.
- W2152629560 cites W2069624343 @default.
- W2152629560 cites W2095915924 @default.
- W2152629560 cites W2096265033 @default.
- W2152629560 cites W2107427955 @default.
- W2152629560 cites W2109100930 @default.
- W2152629560 cites W2112130977 @default.
- W2152629560 cites W2112393517 @default.
- W2152629560 cites W2112630281 @default.
- W2152629560 cites W2112829950 @default.
- W2152629560 cites W2113899819 @default.
- W2152629560 cites W2116355782 @default.
- W2152629560 cites W2117152118 @default.
- W2152629560 cites W2119454022 @default.
- W2152629560 cites W2120413286 @default.
- W2152629560 cites W2132594493 @default.
- W2152629560 cites W2135514503 @default.
- W2152629560 cites W2136108029 @default.
- W2152629560 cites W2136740784 @default.
- W2152629560 cites W2137348488 @default.
- W2152629560 cites W2137864325 @default.
- W2152629560 cites W2139713088 @default.
- W2152629560 cites W2144432042 @default.
- W2152629560 cites W2146297222 @default.
- W2152629560 cites W2153433871 @default.
- W2152629560 cites W2159348063 @default.
- W2152629560 cites W2160721328 @default.
- W2152629560 cites W2165875657 @default.
- W2152629560 cites W2166107621 @default.
- W2152629560 cites W2169558007 @default.
- W2152629560 cites W2170732932 @default.
- W2152629560 cites W2313700577 @default.
- W2152629560 cites W2333657489 @default.
- W2152629560 cites W2335160997 @default.
- W2152629560 cites W3105215077 @default.
- W2152629560 cites W4232120353 @default.
- W2152629560 cites W4244853142 @default.
- W2152629560 cites W75722489 @default.
- W2152629560 doi "https://doi.org/10.1093/gji/ggv069" @default.
- W2152629560 hasPublicationYear "2015" @default.
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