Diverse landscapes beneath Pine Island Glacier influence ice flow

Robert Bingham, David Vaughan, Edward King, Damon Davies, Stephen Cornford, Andrew Smith, Robert Arthern, Alex Brisbourne, Jan De Rydt, Alastair Graham, Matteo Spagnolo, Oliver Marsh, David E Shean

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Abstract

The retreating Pine Island Glacier (PIG), West Antarctica, presently contributes ~5–10% of global sea-level rise. PIG’s retreat rate has increased in recent decades with associated thinning migrating upstream into tributaries feeding the main glacier trunk. To project future change requires modelling that includes robust parameterisation of basal traction, the resistance to ice flow at the bed. However, most ice-sheet models estimate basal traction from satellite-derived surface velocity, without a priori knowledge of the key processes from which it is derived, namely friction at the ice-bed interface and form drag, and the resistance to ice flow that arises as ice deforms to negotiate bed topography. Here, we present high-resolution maps, acquired using ice-penetrating radar, of the bed topography across parts of PIG. Contrary to lower-resolution data currently used for ice-sheet models, these data show a contrasting topography across the ice-bed interface. We show that these diverse subglacial landscapes have an impact on ice flow, and present a challenge for modelling ice-sheet evolution and projecting global sea-level rise from ice-sheet loss.
Original languageEnglish
Article number1618
JournalNature Communications
Volume8
Early online date20 Nov 2017
DOIs
Publication statusPublished - 2017

Fingerprint

Ice Cover
Glaciers
glaciers
Ice
Islands
ice
beds
Traction
Oceans and Seas
Topography
topography
traction
Sea level
Radar
sea level
Friction
tributaries
Antarctic regions
Parameterization
parameterization

Keywords

  • cryospheric science
  • geomorphology
  • geophysics

Cite this

Bingham, R., Vaughan, D., King, E., Davies, D., Cornford, S., Smith, A., ... Shean, D. E. (2017). Diverse landscapes beneath Pine Island Glacier influence ice flow. Nature Communications, 8, [1618]. https://doi.org/10.1038/s41467-017-01597-y

Diverse landscapes beneath Pine Island Glacier influence ice flow. / Bingham, Robert; Vaughan, David; King, Edward; Davies, Damon ; Cornford, Stephen ; Smith, Andrew; Arthern, Robert ; Brisbourne, Alex ; De Rydt, Jan ; Graham, Alastair; Spagnolo, Matteo; Marsh, Oliver ; Shean, David E.

In: Nature Communications, Vol. 8, 1618, 2017.

Research output: Contribution to journalArticle

Bingham, R, Vaughan, D, King, E, Davies, D, Cornford, S, Smith, A, Arthern, R, Brisbourne, A, De Rydt, J, Graham, A, Spagnolo, M, Marsh, O & Shean, DE 2017, 'Diverse landscapes beneath Pine Island Glacier influence ice flow', Nature Communications, vol. 8, 1618. https://doi.org/10.1038/s41467-017-01597-y
Bingham, Robert ; Vaughan, David ; King, Edward ; Davies, Damon ; Cornford, Stephen ; Smith, Andrew ; Arthern, Robert ; Brisbourne, Alex ; De Rydt, Jan ; Graham, Alastair ; Spagnolo, Matteo ; Marsh, Oliver ; Shean, David E. / Diverse landscapes beneath Pine Island Glacier influence ice flow. In: Nature Communications. 2017 ; Vol. 8.
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abstract = "The retreating Pine Island Glacier (PIG), West Antarctica, presently contributes ~5–10{\%} of global sea-level rise. PIG’s retreat rate has increased in recent decades with associated thinning migrating upstream into tributaries feeding the main glacier trunk. To project future change requires modelling that includes robust parameterisation of basal traction, the resistance to ice flow at the bed. However, most ice-sheet models estimate basal traction from satellite-derived surface velocity, without a priori knowledge of the key processes from which it is derived, namely friction at the ice-bed interface and form drag, and the resistance to ice flow that arises as ice deforms to negotiate bed topography. Here, we present high-resolution maps, acquired using ice-penetrating radar, of the bed topography across parts of PIG. Contrary to lower-resolution data currently used for ice-sheet models, these data show a contrasting topography across the ice-bed interface. We show that these diverse subglacial landscapes have an impact on ice flow, and present a challenge for modelling ice-sheet evolution and projecting global sea-level rise from ice-sheet loss.",
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note = "This work was supported by funding from the UK Natural Environment Research Council (NERC) iSTAR Programme (Grants NE/J005665 and NE/K011189), NERC grants NE/B502287/1 and NE/J004766/1 and the British Antarctic Survey (BAS) Polar Science for Planet Earth Programme. D.E.S. was supported by a NASA NESSF fellowship (NNX12AN36H). Bathymetric data used for Fig. 2c and f were sourced from the Bolin Centre Database Oden Mapping Data (cruise OSO 0910; http://oden.geo.su.se/oso0910) and NSF/IEDA Marine Geoscience Data System (http://www.marine-geo.org/tools/search/Files.php?data_set_uid=20080) respectively, and we thank the lead authors M. Jakobsson and F.O. Nitsche for their lodging. All fieldwork was supported by the staff at BAS’s Rothera Research Station and members of the iSTAR Traverse. In particular, we thank James Wake, Tim Gee, Jonny Yates (2013/14), David Routledge (2010/11) and Feargal Buckley, Chris Griffiths and Julian Scott (2007/08) for their help with data acquisition. We thank three anonymous referees for thorough and constructive reviews, which improved the final form of the manuscript.",
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N1 - This work was supported by funding from the UK Natural Environment Research Council (NERC) iSTAR Programme (Grants NE/J005665 and NE/K011189), NERC grants NE/B502287/1 and NE/J004766/1 and the British Antarctic Survey (BAS) Polar Science for Planet Earth Programme. D.E.S. was supported by a NASA NESSF fellowship (NNX12AN36H). Bathymetric data used for Fig. 2c and f were sourced from the Bolin Centre Database Oden Mapping Data (cruise OSO 0910; http://oden.geo.su.se/oso0910) and NSF/IEDA Marine Geoscience Data System (http://www.marine-geo.org/tools/search/Files.php?data_set_uid=20080) respectively, and we thank the lead authors M. Jakobsson and F.O. Nitsche for their lodging. All fieldwork was supported by the staff at BAS’s Rothera Research Station and members of the iSTAR Traverse. In particular, we thank James Wake, Tim Gee, Jonny Yates (2013/14), David Routledge (2010/11) and Feargal Buckley, Chris Griffiths and Julian Scott (2007/08) for their help with data acquisition. We thank three anonymous referees for thorough and constructive reviews, which improved the final form of the manuscript.

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