Extraordinary, 9-day long, global seismic oscillations due to a rockslide-generated tsunami in a Greenland fjord

Paula Koelemeijer, Kristian Svennevig, Stephen Paul Hicks, Thomas Forbriger, Thomas Lecocq, Rudolf Widmer-Schnidrig, Anne Mangeney, C. Hilbert, Niels J. Korsgaard, Antoine Lucas, Claudio Satriano, Robert E. Anthony, Aurelien Mordret, Sven Schippkus, Søren Rysgaard, Wieter Boone, Steven Gibbons, Kristen L. Cook, Sylfest Glimsdal, Finn LøvholtKoen Van Noten, Jelle D. Assink, Alexis Marboeuf, Anthony Lomax, Kris Vanneste, Taka'aki Taira, Matteo Spagnolo, Raphael De Plaen, Carl W. Ebeling, Andrea Cannata, William Harcourt, David G. Cornwell, Corentin Caudron, Pascal Bernard, Piero Poli, Eric Larose, Eleonore Stutzmann, Peter Voss, Björn Lund, Flavio Cannavo, Manuel J. Castro, Esteban Chaves, Trine Dahl-Jensen, Nicolas De Pinho Dias, Aline Déprez, Rouland Develter, Läslo G. Evers, Enrique D. Fernández-Nieto, Ana MG Ferreira, Gareth Funning, Alice-Agnes Gabriel, Marc Hendrickx, Alan L. Kafka, Marie Keiding, Jeffrey Kerby, Shfaqat Abbas Khan, Andreas Kjær Dideriksen, Oliver D. Lamb, Tine Larsen, Bradley Paul Lipovsky, Ikha Magdalena, Jean-Philippe Malet, Mikkel Myrup, Luis A. Rivera, Eugenio Ruiz-Castillo, Selina Wetter, Bastien Wirtz, Douglas Dreger

Publikation: KonferencebidragAbstract ved konferencepeer review

Resumé

Climate change is increasingly predisposing polar regions to large landslides. Tsunamigenic landslides have occurred recently in Greenland, but none have been reported from the eastern fjords. In September 2023, we detected the start of an unprecedented up to 9-day-long global 10.88 mHz (92 s) monochromatic very long-period (VLP) seismic signal, originating from East Greenland. We demonstrate how this event started with a 25 Mm3 glacial thinning-induced rockslide plunging into Dickson Fjord, triggering a 200 m high tsunami. Simulations show the tsunami stabilized into a 7 m-high long-duration seiche with a near-identical frequency (11.45 mHz) and slow amplitude decay as the seismic signal. An oscillating, fjord-transverse single-force with a maximum amplitude of 5×1011 N reproduces the seismic amplitudes and their radiation pattern relative to the fjord, demonstrating how a seiche directly caused the 9-day long seismic signal. Our findings highlight how climate change is causing cascading, hazardous feedbacks between the cryosphere, hydrosphere and lithosphere.
OriginalsprogEngelsk
StatusUdgivet - 9 dec. 2024
BegivenhedAmerican Geophysical Union annual meeting 2024 - Washington D.C., USA
Varighed: 9 dec. 202413 dec. 2024
https://www.agu.org/annual-meeting

Konference

KonferenceAmerican Geophysical Union annual meeting 2024
Forkortet titelAGU24
Land/OmrådeUSA
ByWashington D.C.
Periode9/12/2413/12/24
Internetadresse

Programområde

  • Programområde 3: Energiressourcer
  • Programområde 4: Mineralske råstoffer
  • Programområde 5: Natur og klima

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