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1000 Titel
  • Misidentified subglacial lake beneath the Devon Ice Cap, Canadian Arctic: a new interpretation from seismic and electromagnetic data
1000 Autor/in
  1. Killingbeck, Siobhan F. |
  2. Rutishauser, Anja |
  3. Unsworth, Martyn J. |
  4. Dubnick, Ashley |
  5. Criscitiello, Alison S. |
  6. Killingbeck, James |
  7. Dow, Christine F. |
  8. Hill, Tim |
  9. Booth, Adam D. |
  10. Main, Brittany |
  11. Brossier, Eric |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-08-20
1000 Erschienen in
1000 Quellenangabe
  • 18(8):3699-3722
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-3699-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. In 2018 the first subglacial lake in the Canadian Arctic was proposed to exist beneath the Devon Ice Cap, based on the analysis of airborne radar data. Here, we report a new interpretation of the subglacial material beneath the Devon Ice Cap, supported by data acquired from multiple surface-based geophysical methods in 2022. The geophysical data recorded included 9 km of active-source seismic-reflection profiles, seven transient electromagnetic (TEM) soundings, and 17 magnetotellurics (MT) stations. These surface-based geophysical datasets were collected above the inferred locations of the subglacial lakes and show no evidence for the presence of subglacial water. The acoustic impedance of the subglacial material, estimated from the seismic data, is 9.49 ± 1.92 × 106 kg m−2 s−1, comparable to consolidated or frozen sediment. The resistivity models obtained by inversion of both the TEM and MT measurements show the presence of highly resistive rock layers (1000–100 000 Ω m) directly beneath the ice. Re-evaluation of the airborne reflectivity data shows that the radar attenuation rates were likely overestimated, leading to an overestimation of the basal reflectivity in the original radar studies. Here, we derive new radar attenuation rates using the temperature- and chemistry-dependent Arrhenius equation, and when applied to correct the returned bed power, the bed power does not meet the basal reflectivity threshold expected over subglacial water. Thus, the radar interpretation is now consistent with the seismic and electromagnetic observations of dry or frozen, non-conductive basal material. </jats:p>
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/S2lsbGluZ2JlY2ssIFNpb2JoYW4gRi4=|https://frl.publisso.de/adhoc/uri/UnV0aXNoYXVzZXIsIEFuamE=|https://frl.publisso.de/adhoc/uri/VW5zd29ydGgsIE1hcnR5biBKLg==|https://frl.publisso.de/adhoc/uri/RHVibmljaywgQXNobGV5|https://frl.publisso.de/adhoc/uri/Q3Jpc2NpdGllbGxvLCBBbGlzb24gUy4=|https://frl.publisso.de/adhoc/uri/S2lsbGluZ2JlY2ssIEphbWVz|https://frl.publisso.de/adhoc/uri/RG93LCBDaHJpc3RpbmUgRi4=|https://frl.publisso.de/adhoc/uri/SGlsbCwgVGlt|https://frl.publisso.de/adhoc/uri/Qm9vdGgsIEFkYW0gRC4=|https://frl.publisso.de/adhoc/uri/TWFpbiwgQnJpdHRhbnk=|https://frl.publisso.de/adhoc/uri/QnJvc3NpZXIsIEVyaWM=
1000 Hinweis
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1000 Label
1000 Förderer
  1. Weston Family Foundation |
  2. Natural Sciences and Engineering Research Council of Canada |
1000 Fördernummer
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  2. -
1000 Förderprogramm
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  2. -
1000 Dateien
1000 Förderung
  1. 1000 joinedFunding-child
    1000 Förderer Weston Family Foundation |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer Natural Sciences and Engineering Research Council of Canada |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
1000 Beschrieben durch
1000 @id frl:6488086.rdf
1000 Erstellt am 2024-10-03T09:56:21.278+0200
1000 Erstellt von 322
1000 beschreibt frl:6488086
1000 Zuletzt bearbeitet 2024-10-04T15:13:03.214+0200
1000 Objekt bearb. Fri Oct 04 15:13:03 CEST 2024
1000 Vgl. frl:6488086
1000 Oai Id
  1. oai:frl.publisso.de:frl:6488086 |
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