Articles | Volume 14, issue 1
https://doi.org/10.5194/tc-14-261-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-261-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Glacial sedimentation, fluxes and erosion rates associated with ice retreat in Petermann Fjord and Nares Strait, north-west Greenland
British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UK
Center for Coastal and Ocean Mapping, University of New Hampshire,
Durham, NH 03824, USA
Martin Jakobsson
Department of Geological Sciences, Stockholm University, 106 91
Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, 106 91
Stockholm, Sweden
Larry Mayer
Center for Coastal and Ocean Mapping, University of New Hampshire,
Durham, NH 03824, USA
Brendan T. Reilly
College of Earth, Ocean, and Atmospheric Sciences, Oregon State
University, Corvallis, OR 97331, USA
Anne E. Jennings
Institute of Arctic and Alpine Research, University of Colorado,
Boulder, CO 80309-0450, USA
Joseph S. Stoner
College of Earth, Ocean, and Atmospheric Sciences, Oregon State
University, Corvallis, OR 97331, USA
Tove Nielsen
Geological Survey of Denmark and Greenland, Øster Voldgade 10,
1350 Copenhagen K, Denmark
Katrine J. Andresen
Department of Geoscience, Aarhus University, Hoegh-Guldbergs Gade 2, 8000, Aarhus C, Denmark
Egon Nørmark
Department of Geoscience, Aarhus University, Hoegh-Guldbergs Gade 2, 8000, Aarhus C, Denmark
Katrien A. Heirman
Geological Survey of Denmark and Greenland, Øster Voldgade 10,
1350 Copenhagen K, Denmark
TNO, Geological Survey of the Netherlands, Princetonlaan 6, 3584
CB Utrecht, the Netherlands
Elina Kamla
Geological Survey of Denmark and Greenland, Øster Voldgade 10,
1350 Copenhagen K, Denmark
Rambøll Management Consulting, Hannemanns Allé 53, 2300
Copenhagen S, Denmark
Kevin Jerram
Center for Coastal and Ocean Mapping, University of New Hampshire,
Durham, NH 03824, USA
Christian Stranne
Department of Geological Sciences, Stockholm University, 106 91
Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, 106 91
Stockholm, Sweden
Alan Mix
College of Earth, Ocean, and Atmospheric Sciences, Oregon State
University, Corvallis, OR 97331, USA
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- Modern foraminiferal assemblages in northern Nares Strait, Petermann Fjord, and beneath Petermann ice tongue, NW Greenland A. Jennings et al. 10.1080/15230430.2020.1806986
- Sediment Provenance in the Baker-Martínez Fjord System (Chile, 48°S) Indicated by Magnetic Susceptibility and Inorganic Geochemistry M. Troch et al. 10.3389/fmars.2021.612309
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- Sediment fill of Baffin Island fjords: Architecture and rates J. Syvitski et al. 10.1016/j.quascirev.2022.107474
- Retreat and stabilization of a marine-based ice margin along a high arctic fjord-cross-shelf trough system P. Couette et al. 10.1016/j.quascirev.2022.107949
- Centennial‐ and Orbital‐Scale Erosion Beneath the Greenland Ice Sheet Near Jakobshavn Isbræ A. Balter‐Kennedy et al. 10.1029/2021JF006429
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- Towards modelling of corrugation ridges at ice-sheet grounding lines K. Hogan et al. 10.5194/tc-17-2645-2023
- Late Weichselian and Holocene behavior of the Greenland Ice Sheet in the Kejser Franz Josef Fjord system, NE Greenland I. Olsen et al. 10.1016/j.quascirev.2022.107504
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Latest update: 10 Oct 2024
Short summary
Glacial sediments in fjords hold a key record of environmental and ice dynamic changes during ice retreat. Here we use a comprehensive geophysical survey from the Petermann Fjord system in NW Greenland to map these sediments, identify depositional processes and calculate glacial erosion rates for the retreating palaeo-Petermann ice stream. Ice streaming is the dominant control on glacial erosion rates which vary by an order of magnitude during deglaciation and are in line with modern rates.
Glacial sediments in fjords hold a key record of environmental and ice dynamic changes during...