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• W1969227012 abstract "[1] Contributions to sea level rise from rapidly retreating marine-terminating glaciers are large and increasing. Strong increases in iceberg calving occur during retreat, which allows mass transfer to the ocean at a much higher rate than possible through surface melt alone. To study this process, we deployed an 11-sensor passive seismic network at Columbia Glacier, Alaska, during 2004–2005. We show that calving events generate narrow-band seismic signals, allowing frequency domain detections. Detection parameters were determined using direct observations of calving and validated using three statistical methods and hypocenter locations. The 1–3 Hz detections provide a good measure of the temporal distribution and size of calving events. Possible source mechanisms for the unique waveforms are discussed, and we analyze potential forcings for the observed seismicity." @default.
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• W1969227012 date "2007-05-03" @default.
• W1969227012 modified "2023-10-17" @default.
• W1969227012 title "Seismic detection and analysis of icequakes at Columbia Glacier, Alaska" @default.
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• W1969227012 doi "https://doi.org/10.1029/2006jf000595" @default.
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