Articles | Volume 15, issue 3
https://doi.org/10.5194/tc-15-1435-2021
© Author(s) 2021. 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-15-1435-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Basal traction mainly dictated by hard-bed physics over grounded regions of Greenland
IGE, Université Grenoble Alpes, CNRS, Grenoble, France
Florent Gimbert
IGE, Université Grenoble Alpes, CNRS, Grenoble, France
Fabien Gillet-Chaulet
IGE, Université Grenoble Alpes, CNRS, Grenoble, France
Adrien Gilbert
IGE, Université Grenoble Alpes, CNRS, Grenoble, France
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Internal climate variability, resulting from processes intrinsic to the climate system, modulates the Antarctic response to climate change by delaying or offsetting its effects. Using climate and ice-sheet models, we highlight that irreducible internal climate variability significantly enlarges the likely range of Antarctic contribution to sea-level rise until 2100. Thus, we recommend considering internal climate variability as a source of uncertainty for future ice-sheet projections.
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The flow of glaciers and ice sheets results from ice deformation and basal sliding driven by gravitational forces. Quantifying the rate at which ice deforms under its own weight is critical for assessing glacier evolution. This study uses borehole instrumentation in an Alpine glacier to quantify ice deformation and constrain ice viscosity in a natural setting. Our results show that the viscosity of ice at 0 °C is largely influenced by interstitial liquid water, which enhances ice deformation.
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Inspired by a previous intercomparison framework, our study better constrains uncertainties in glacier evolution using an innovative method to validate Bayesian calibration. Upernavik Isstrøm, one of Greenland's largest glaciers, has lost significant mass since 1985. By integrating observational data, climate models, human emissions, and internal model parameters, we project its evolution until 2100. We show that future human emissions are the main source of uncertainty in 2100, making up half.
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Małgorzata Chmiel, Maxime Godano, Marco Piantini, Pierre Brigode, Florent Gimbert, Maarten Bakker, Françoise Courboulex, Jean-Paul Ampuero, Diane Rivet, Anthony Sladen, David Ambrois, and Margot Chapuis
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On 2 October 2020, the French Maritime Alps were struck by an extreme rainfall event caused by Storm Alex. Here, we show that seismic data provide the timing and velocity of the propagation of flash-flood waves along the Vésubie River. We also detect 114 small local earthquakes triggered by the rainwater weight and/or its infiltration into the ground. This study paves the way for future works that can reveal further details of the impact of Storm Alex on the Earth’s surface and subsurface.
Anna Derkacheva, Fabien Gillet-Chaulet, Jeremie Mouginot, Eliot Jager, Nathan Maier, and Samuel Cook
The Cryosphere, 15, 5675–5704, https://doi.org/10.5194/tc-15-5675-2021, https://doi.org/10.5194/tc-15-5675-2021, 2021
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Along the edges of the Greenland Ice Sheet surface melt lubricates the bed and causes large seasonal fluctuations in ice speeds during summer. Accurately understanding how these ice speed changes occur is difficult due to the inaccessibility of the glacier bed. We show that by using surface velocity maps with high temporal resolution and numerical modelling we can infer the basal conditions that control seasonal fluctuations in ice speed and gain insight into seasonal dynamics over large areas.
Marco Piantini, Florent Gimbert, Hervé Bellot, and Alain Recking
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We carry out laboratory experiments to investigate the formation and propagation dynamics of exogenous sediment pulses in mountain rivers. We show that the ability of a self-formed deposit to destabilize and generate sediment pulses depends on the sand content of the mixture, while each pulse turns out to be formed by a front, a body, and a tail. Seismic measurements reveal a complex and non-unique dependency between seismic power and sediment pulse transport characteristics.
Chloé Scholzen, Thomas V. Schuler, and Adrien Gilbert
The Cryosphere, 15, 2719–2738, https://doi.org/10.5194/tc-15-2719-2021, https://doi.org/10.5194/tc-15-2719-2021, 2021
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We use a two-dimensional model of water flow below the glaciers in Kongsfjord, Svalbard, to investigate how different processes of surface-to-bed meltwater transfer affect subglacial hydraulic conditions. The latter are important for the sliding motion of glaciers, which in some cases exhibit huge variations. Our findings indicate that the glaciers in our study area undergo substantial sliding because water is poorly evacuated from their base, with limited influence from the surface hydrology.
Andreas Kääb, Mylène Jacquemart, Adrien Gilbert, Silvan Leinss, Luc Girod, Christian Huggel, Daniel Falaschi, Felipe Ugalde, Dmitry Petrakov, Sergey Chernomorets, Mikhail Dokukin, Frank Paul, Simon Gascoin, Etienne Berthier, and Jeffrey S. Kargel
The Cryosphere, 15, 1751–1785, https://doi.org/10.5194/tc-15-1751-2021, https://doi.org/10.5194/tc-15-1751-2021, 2021
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Hardly recognized so far, giant catastrophic detachments of glaciers are a rare but great potential for loss of lives and massive damage in mountain regions. Several of the events compiled in our study involve volumes (up to 100 million m3 and more), avalanche speeds (up to 300 km/h), and reaches (tens of kilometres) that are hard to imagine. We show that current climate change is able to enhance associated hazards. For the first time, we elaborate a set of factors that could cause these events.
Christian Vincent, Diego Cusicanqui, Bruno Jourdain, Olivier Laarman, Delphine Six, Adrien Gilbert, Andrea Walpersdorf, Antoine Rabatel, Luc Piard, Florent Gimbert, Olivier Gagliardini, Vincent Peyaud, Laurent Arnaud, Emmanuel Thibert, Fanny Brun, and Ugo Nanni
The Cryosphere, 15, 1259–1276, https://doi.org/10.5194/tc-15-1259-2021, https://doi.org/10.5194/tc-15-1259-2021, 2021
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In situ glacier point mass balance data are crucial to assess climate change in different regions of the world. Unfortunately, these data are rare because huge efforts are required to conduct in situ measurements on glaciers. Here, we propose a new approach from remote sensing observations. The method has been tested on the Argentière and Mer de Glace glaciers (France). It should be possible to apply this method to high-spatial-resolution satellite images and on numerous glaciers in the world.
Vincent Peyaud, Coline Bouchayer, Olivier Gagliardini, Christian Vincent, Fabien Gillet-Chaulet, Delphine Six, and Olivier Laarman
The Cryosphere, 14, 3979–3994, https://doi.org/10.5194/tc-14-3979-2020, https://doi.org/10.5194/tc-14-3979-2020, 2020
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Alpine glaciers are retreating at an accelerating rate in a warming climate. Numerical models allow us to study and anticipate these changes, but the performance of a model is difficult to evaluate. So we compared an ice flow model with the long dataset of observations obtained between 1979 and 2015 on Mer de Glace (Mont Blanc area). The model accurately reconstructs the past evolution of the glacier. We simulate the future evolution of Mer de Glace; it could retreat by 2 to 6 km by 2050.
Cited articles
Alley, R. B. and Joughin, I.: Modeling Ice-Sheet Flow, Science, 336,
551–552, 2012.
Bons, P. D., Kleiner, T., Llorens, M., Prior, D. J., Sachau, T., Weikusat,
I., and Jansen, D.: Greenland Ice Sheet: Higher nonlinearity of ice flow
significantly reduces estimated basal motion, Geophys. Res. Lett.,
45, 6542–6548, 2018.
Booth, A. D., Clark, R. A., Kulessa, B., Murray, T., Carter, J., Doyle, S., and Hubbard, A.: Thin-layer effects in glaciological seismic amplitude-versus-angle (AVA) analysis: implications for characterising a subglacial till unit, Russell Glacier, West Greenland, The Cryosphere, 6, 909–922, https://doi.org/10.5194/tc-6-909-2012, 2012.
Bougamont, M., Christoffersen, P., Hubbard, A., Fitzpatrick, A., Doyle, S., and Carter, S.: Sensitive response of the Greenland Ice Sheet to surface melt drainage over a soft bed, Nat. Commun., 5, 19, https://doi.org/10.1038/ncomms6052, 2014.
Carr, J. R., Vieli, A., Stokes, C., Jamieson, S., Palmer, S.,
Christoffersen, P., Dowdeswell, J., Nick, F., Blankenship, D. D., and Young,
D. A.: Basal topographic controls on rapid retreat of Humboldt Glacier,
northern Greenland, J. Glaciol., 61, 137–150, 2015.
Cavanagh, J., Lampkin, D., and Moon, T.: Seasonal variability in regional ice
flow due to meltwater injection into the shear margins of Jakobshavn
Isbræ, J. Geophys. Res.-Earth, 122,
2488–2505, 2017.
Christianson, K., Peters, L. E., Alley, R. B., Anandakrishnan, S., Jacobel,
R. W., Riverman, K. L., Muto, A., and Keisling, B. A.: Dilatant till
facilitates ice-stream flow in northeast Greenland, Earth Planet.
Sc. Lett., 401, 57–69, 2014.
Cooper, M. A., Jordan, T. M., Schroeder, D. M., Siegert, M. J., Williams, C. N., and Bamber, J. L.: Subglacial roughness of the Greenland Ice Sheet: relationship with contemporary ice velocity and geology, The Cryosphere, 13, 3093–3115, https://doi.org/10.5194/tc-13-3093-2019, 2019.
Csatho, B. M., Schenk, A. F., van der Veen, C. J., Babonis, G., Duncan, K.,
Rezvanbehbahani, S., Van Den Broeke, M. R., Simonsen, S. B., Nagarajan, S.,
and van Angelen, J. H.: Laser altimetry reveals complex pattern of Greenland
Ice Sheet dynamics, P. Natl. Acad. Sci. USA,
111, 18478–18483, 2014.
Cuffey, K. M. and Paterson, W. S. B.: The Physics of Glaciers, Academic
Press, Burlington, MA, Butterworth-Heinemann/Elsevier, 721 pp., 2010.
Dahl-Jensen, D. and Gundestrup, N.: Constitutive properties of ice at Dye 3,
Greenland, International Association of Hydrological Sciences Publication,
170, 31–43, 1987.
Das, S. B., Joughin, I., Behn, M. D., Howat, I. M., King, M. A., Lizarralde,
D., and Bhatia, M. P.: Fracture propagation to the base of the Greenland Ice
Sheet during supraglacial lake drainage, Science, 320, 778–781, 2008.
Dow, C. F., Hubbard, A., Booth, A. D., Doyle, S. H., Gusmeroli, A., and
Kulessa, B.: Seismic evidence of mechanically weak sediments underlying
Russell Glacier, West Greenland, Ann. Glaciol., 54, 135–141,
2013.
Doyle, S. H., Hubbard, B., Christoffersen, P., Young, T. J., Hofstede, C.,
Bougamont, M., Box, J., and Hubbard, A.: Physical conditions of fast glacier
flow: 1. Measurements from boreholes drilled to the bed of Store Glacier,
West Greenland, J. Geophys. Res.-Earth, 123,
324–348, 2018.
Fahnestock, M., Abdalati, W., Joughin, I., Brozena, J., and Gogineni, P.:
High geothermal heat flow, basal melt, and the origin of rapid ice flow in
central Greenland, Science, 294, 2338–2342, 2001.
Gagliardini, O., Cohen, D., Råback, P., and Zwinger, T.: Finite-element
modeling of subglacial cavities and related friction law, J.
Geophys. Res.-Earth, 112, F02027, https://doi.org/10.1029/2006JF000576, 2007.
Gagliardini, O., Zwinger, T., Gillet-Chaulet, F., Durand, G., Favier, L., de Fleurian, B., Greve, R., Malinen, M., Martín, C., Råback, P., Ruokolainen, J., Sacchettini, M., Schäfer, M., Seddik, H., and Thies, J.: Capabilities and performance of Elmer/Ice, a new-generation ice sheet model, Geosci. Model Dev., 6, 1299–1318, https://doi.org/10.5194/gmd-6-1299-2013, 2013.
Gillet-Chaulet, F., Hindmarsh, R. C., Corr, H. F., King, E. C., and Jenkins,
A.: In-situquantification of ice rheology and direct measurement of the
Raymond Effect at Summit, Greenland using a phase-sensitive radar,
Geophys. Res. Lett., 38, L24503, https://doi.org/10.1029/2011GL049843, 2011.
Gillet-Chaulet, F., Durand, G., Gagliardini, O., Mosbeux, C., Mouginot, J.,
Rémy, F., and Ritz, C.: Assimilation of surface velocities acquired
between 1996 and 2010 to constrain the form of the basal friction law under
Pine Island Glacier, Geophys. Res. Lett., 43, 10–311, 2016.
Goelzer, H., Robinson, A., Seroussi, H., and van de Wal, R. S. W.: Recent
Progress in Greenland Ice Sheet Modelling, Curr. Clim. Change Rep., 3,
291–302, 2017.
Habermann, M., Truffer, M., and Maxwell, D.: Changing basal conditions during the speed-up of Jakobshavn Isbræ, Greenland, The Cryosphere, 7, 1679–1692, https://doi.org/10.5194/tc-7-1679-2013, 2013.
Harper, J. T., Humphrey, N. F., Meierbachtol, T. W., Graly, J. A., and
Fischer, U. H.: Borehole measurements indicate hard bed conditions,
Kangerlussuaq sector, western Greenland Ice Sheet, J. Geophys.
Res.-Earth, 122, 1605–1618, 2017.
Harrington, J. A., Humphrey, N. F., and Harper, J. T.: Temperature
distribution and thermal anomalies along a flowline of the Greenland ice
sheet, Ann. Glaciol., 56, 98–104, 2015.
Hogg, A. E., Shepherd, A., Gourmelen, N., and Engdahl, M.: Grounding line
migration from 1992 to 2011 on Petermann Glacier, north-west Greenland,
J. Glaciol., 62, 1104–1114, 2016.
Howat, I. M., Negrete, A., and Smith, B. E.: The Greenland Ice Mapping Project (GIMP) land classification and surface elevation data sets, The Cryosphere, 8, 1509–1518, https://doi.org/10.5194/tc-8-1509-2014, 2014.
Howat, I., Negrete, A., and Smith, B.: MEaSUREs Greenland Ice Mapping Project
(GIMP) Digital Elevation Model from GeoEye and WorldView Imagery, Version
1, Boulder, Colorado USA, NASA National Snow and Ice Data Center
Distributed Active Archive Center, https://doi.org/10.5067/H0KUYVF53Q8M,
2017.
Iken, A.: The Effect of the Subglacial Water Pressure on the Sliding
Velocity of a Glacier in an Idealized Numerical Model, J.
Glaciol., 27, 407–421, https://doi.org/10.3189/S0022143000011448,
1981.
Iverson, N. R., Hooyer, T. S., and Baker, R. W.: Ring-shear studies of till
deformation: Coulomb-plastic behavior and distributed strain in glacier
beds, J. Glaciol., 44, 634–642, 1998.
Iverson, N. R., Cohen, D., Hooyer, T. S., Fischer, U. H., Jackson, M.,
Moore, P. L., Lappegard, G., and Kohler, J.: Effects of basal debris on
glacier flow, Science, 301, 81–84, 2003.
Joughin, I., MacAyeal, D. R., and Tulaczyk, S.: Basal shear stress of the
Ross ice streams from control method inversions, J. Geophys.
Res.-Sol. Ea., 109, B09405, https://doi.org/10.1029/2003JB002960, 2004.
Joughin, I., Smith, B. E., Howat, I. M., Floricioiu, D., Alley, R. B.,
Truffer, M., and Fahnestock, M.: Seasonal to decadal scale variations in the
surface velocity of Jakobshavn Isbrae, Greenland: Observation and
model-based analysis, J. Geophys. Res.-Earth,
117, F02030, https://doi.org/10.1029/2011JF002110, 2012.
Joughin, I., Smith, B., Howat, I., and Scambos, T.: MEaSUREs Multi-year
Greenland Ice Sheet Velocity Mosaic, Version 1, Boulder, Colorado USA, NASA
National Snow and Ice Data Center Distributed Active Archive Center,
https://doi.org/10.5067/QUA5Q9SVMSJG, 2016.
Joughin, I., Smith, B. E., and Howat, I. M.: A complete map of Greenland ice
velocity derived from satellite data collected over 20 years, J.
Glaciol., 64, 1–11, 2018.
Joughin, I., Smith, B. E., and Schoof, C. G.: Regularized Coulomb friction
laws for ice sheet sliding: application to Pine Island Glacier, Antarctica,
Geophys. Res. Lett., 46, 4764–4771, 2019.
Kääb, A., Leinss, S., Gilbert, A., Bühler, Y., Gascoin, S.,
Evans, S. G., Bartelt, P., Berthier, E., Brun, F., and Chao, W.-A.: Massive
collapse of two glaciers in western Tibet in 2016 after surge-like
instability, Nat. Geosci., 11, 114–120, 2018.
Kamb, B.: Rheological nonlinearity and flow instability in the deforming bed
mechanism of ice stream motion, J. Geophys. Res.-Sol.
Ea., 96, 16585–16595, 1991.
Kulessa, B., Hubbard, A. L., Booth, A. D., Bougamont, M., Dow, C. F., Doyle,
S. H., Christoffersen, P., Lindbäck, K., Pettersson, R., Fitzpatrick, A.
A. W., and Jones, G. A.: Seismic evidence for complex sedimentary control of
Greenland Ice Sheet flow, Sci. Adv., 3, e1603071, https://doi.org/10.1126/sciadv.1603071, 2017.
Kyrke-Smith, T. M., Gudmundsson, G. H., and Farrell, P. E.: Relevance of
detail in basal topography for basal slipperiness inversions: a case study
on Pine Island Glacier, Antarctica, Front. Earth Sci., 6, 33, https://doi.org/10.3389/feart.2018.00033, 2018.
Lampkin, D., Amador, N., Parizek, B., Farness, K., and Jezek, K.: Drainage
from water-filled crevasses along the margins of Jakobshavn Isbræ: A
potential catalyst for catchment expansion, J. Geophys. Res.-Earth, 118, 795–813, 2013.
Leeson, A., Shepherd, A., Briggs, K., Howat, I., Fettweis, X., Morlighem, M.,
and Rignot, E.: Supraglacial lakes on the Greenland ice sheet advance inland
under warming climate, Nat. Clim. Change, 5, 51–55, 2015.
Lindbäck, K. and Pettersson, R.: Spectral roughness and glacial erosion
of a land-terminating section of the Greenland Ice Sheet, Geomorphology,
238, 149–159, 2015.
Lliboutry, L.: General Theory of Subglacial Cavitation and Sliding of
Temperate Glaciers, J. Glaciol., 7, 21–58, 1968.
Lüthi, M., Funk, M., Iken, A., Gogineni, S., and Truffer, M.: Mechanisms
of fast flow in Jakobshavn Isbræ, West Greenland: Part III. Measurements
of ice deformation, temperature and cross-borehole conductivity in boreholes
to the bedrock, J. Glaciol., 48, 369–385, 2002.
Lüthi, M. P., Ryser, C., Andrews, L. C., Catania, G. A., Funk, M., Hawley, R. L., Hoffman, M. J., and Neumann, T. A.: Heat sources within the Greenland Ice Sheet: dissipation, temperate paleo-firn and cryo-hydrologic warming, The Cryosphere, 9, 245–253, https://doi.org/10.5194/tc-9-245-2015, 2015.
MacAyeal, D. R.: Large-scale ice flow over a viscous basal sediment: Theory
and application to ice stream B, Antarctica, J. Geophys.
Res.-Sol. Ea., 94, 4071–4087, 1989.
MacGregor, J., Fahnestock, M. A., Catania, G. A., Aschwanden, A., Clow, G.
D., Colgan, W. T., Gogineni, S. P., Morlighem, M., Nowicki, S. M. J., Paden,
J. D., Price, S. F., and Seroussi, H.: A synthesis of the basal thermal state
of the Greenland Ice Sheet, J. Geophys. Res.-Earth,
121, 1328–1350, 2016.
MacGregor, J., Fahnestock, M., Catania, G., Paden, J., Gogineni, P.,
Morlighem, M., Colgan, W., Nowicki, S. M., Clow, G., Aschwanden, A., Price,
S. F., and Seroussi, H.: Likely Basal Thermal State of the Greenland Ice
Sheet, Version 1, Boulder, Colorado USA, NASA National Snow and Ice Data
Center Distributed Active Archive Center,
https://doi.org/10.5067/R4MWDWWUWQF9, 2017.
Maier, N., Humphrey, N., Harper, J., and Meierbachtol, T.: Sliding dominates
slow-flowing margin regions, Greenland Ice Sheet, Sci. Adv., 5,
eaaw540, https://doi.org/10.1126/sciadv.aaw5406, 2019.
McCormack, F. S., Roberts, J. L., Jong, L. M., Young, D. A., and Beem, L. H.:
A note on digital elevation model smoothing and driving stresses, Polar
Res., 38, https://doi.org/10.33265/polar.v38.3498, 2019.
Meierbachtol, T., Harper, J., and Johnson, J.: Force Balance along Isunnguata
Sermia, West Greenland, Front. Earth Sci., 4, 87, https://doi.org/10.3389/feart.2016.00087, 2016.
Minchew, B., Simons, M., Björnsson, H., Pálsson, F., Morlighem, M.,
Seroussi, H., Larour, E., and Hensley, S.: Plastic bed beneath Hofsjökull
Ice Cap, central Iceland, and the sensitivity of ice flow to surface
meltwater flux, J. Glaciol., 62, 147–158, 2016.
Minchew, B., Meyer, C. R., Pegler, S. S., Lipovsky, B. P., Rempel, A. W.,
Gudmundsson, G. H., and Iverson, N. R.: Comment on “Friction at the bed does
not control fast glacier flow”, Science, 363, eaau6055, https://doi.org/10.1126/science.aau6055, 2019.
Morland, L. and Johnson, I.: Steady motion of ice sheets, J.
Glaciol., 25, 229–246, 1980.
Morlighem, M.: IceBridge BedMachine Greenland, Version 3, Boulder, Colorado
USA, NASA National Snow and Ice Data Center Distributed Active Archive
Center, https://doi.org/10.5067/2CIX82HUV88Y, 2018.
Morlighem, M., Rignot, E., Seroussi, H., Larour, E., Ben Dhia, H., and Aubry,
D.: Spatial patterns of basal drag inferred using control methods from a
full-Stokes and simpler models for Pine Island Glacier, West Antarctica,
Geophys. Res. Lett., 37, L14502, https://doi.org/10.1029/2010GL043853, 2010.
Morlighem, M., Williams, C. N., Rignot, E., An, L., Arndt, J. E., Bamber, J.
L., Catania, G., Chauché, N., Dowdeswell, J. A., and Dorschel, B.:
BedMachine v3: Complete bed topography and ocean bathymetry mapping of
Greenland from multibeam echo sounding combined with mass conservation,
Geophys. Res. Lett., 44, 11051–11061, https://doi.org/10.1002/2017GL074954, 2017.
Mouginot, J., Rignot, E., Bjørk, A. A., Van Den Broeke, M., Millan, R.,
Morlighem, M., Noël, B., Scheuchl, B., and Wood, M.: Forty-six years of
Greenland Ice Sheet mass balance from 1972 to 2018, P.
Natl. Acad. Sci. USA, 116, 9239–9244, 2019.
Poinar, K., Joughin, I., Das, S. B., Behn, M. D., Lenaerts, J. T., and Van
Den Broeke, M. R.: Limits to future expansion of surface-melt-enhanced ice
flow into the interior of western Greenland, Geophys. Res. Lett.,
42, 1800–1807, 2015.
Rippin, D. M.: Bed roughness beneath the Greenland ice sheet, J.
Glaciol., 59, 724–732, 2013.
Rogozhina, I., Petrunin, A. G., Vaughan, A. P., Steinberger, B., Johnson, J.
V., Kaban, M. K., Calov, R., Rickers, F., Thomas, M., and Koulakov, I.:
Melting at the base of the Greenland ice sheet explained by Iceland hotspot
history, Nat. Geosci., 9, 366–369, 2016.
Ryser, C., Lüthi, M. P., Andrews, L. C., Hoffman, M. J., Catania, G. A.,
and Hawley, R. L.: Sustained high basal motion of the Greenland ice sheet
revealed by borehole deformation, J. Glaciol., 60, 647660, https://doi.org/10.3189/2014JoG13J196, 2014.
Schoof, C.: The effect of cavitation on glacier sliding, P.
Roy. Soc. A-Math. Phys., 461,
609–627, 2005.
Seddik, H., Greve, R., Zwinger, T., Gillet-Chaulet, F., and Gagliardini, O.:
Simulations of the Greenland ice sheet 100 years into the future with the
full Stokes model Elmer/Ice, J. Glaciol., 58, 427–440, 2012.
Shapero, D. R., Joughin, I. R., Poinar, K., Morlighem, M., and
Gillet-Chaulet, F.: Basal resistance for three of the largest Greenland
outlet glaciers, J. Geophys. Res.-Earth, 121,
168–180, 2016.
Smith, L. C., Chu, V. W., Yang, K., Gleason, C. J., Pitcher, L. H.,
Rennermalm, A. K., Legleiter, C. J., Behar, A. E., Overstreet, B. T.,
Moustafa, S. E., Tedesco, M., Forster, R. R., LeWinter, A. L., Finnegan, D.
C., Sheng, Y., and Balog, J.: Efficient meltwater drainage through
supraglacial streams and rivers on the southwest Greenland ice sheet, P.
Natl. Acad. Sci. USA, 112, 1001, https://doi.org/10.1073/pnas.1413024112, 2015.
Stearns, L. A. and van der Veen, C. J.: Friction at the bed does not control
fast glacier flow, Science, 361, 273–277,
https://doi.org/10.1126/science.aat2217, 2018.
Stearns, L. A. and van der Veen, C.: Response to Comment on “Friction at
the bed does not control fast glacier flow”, Science, 363, eaau8375, https://doi.org/10.1126/science.aau8375,
2019.
Stevens, L. A., Behn, M. D., McGuire, J. J., Das, S. B., Joughin, I.,
Herring, T., Shean, D. E., and King, M. A.: Greenland supraglacial lake
drainages triggered by hydrologically induced basal slip, Nature, 522,
73–76, 2015.
Tulaczyk, S.: Ice sliding over weak, fine-grained tills: Dependence of
ice-till interactions on till granulometry, Geol. S. Am. S., 337, 159, https://doi.org/10.1130/0-8137-2337-X.159, 1999.
Tulaczyk, S. M., Scherer, R. P., and Clark, C. D.: A ploughing model for the
origin of weak tills beneath ice streams: a qualitative treatment,
Quaternary Int., 86, 59–70, 2001.
Vandecrux, B., MacFerrin, M., Machguth, H., Colgan, W. T., van As, D., Heilig, A., Stevens, C. M., Charalampidis, C., Fausto, R. S., Morris, E. M., Mosley-Thompson, E., Koenig, L., Montgomery, L. N., Miège, C., Simonsen, S. B., Ingeman-Nielsen, T., and Box, J. E.: Firn data compilation reveals widespread decrease of firn air content in western Greenland, The Cryosphere, 13, 845–859, https://doi.org/10.5194/tc-13-845-2019, 2019.
Walter, F., Chaput, J., and Lüthi, M. P.: Thick sediments beneath
Greenland's ablation zone and their potential role in future ice sheet
dynamics, Geology, 42, 487–490, 2014.
Weertman, J.: The Theory of Glacier Sliding, J. Glaciol., 5,
287–303, 1964.
Wright, P. J., Harper, J. T., Humphrey, N. F., and Meierbachtol, T. W.:
Measured basal water pressure variability of the western Greenland Ice
Sheet: Implications for hydraulic potential, J. Geophys.
Res.-Earth, 121, 1134–1147, 2016.
Zoet, L. K. and Iverson, N. R.: A slip law for glaciers on deformable beds,
Science, 368, 76–78, 2020.
Zwally, H. J., Giovinetto, M. B., Beckley, M. A., and Saba, J. L.: Antarctic
and Greenland drainage systems, GSFC cryospheric sciences laboratory,
available at: https://icesat4.gsfc.nasa.gov/cryo_data/ant_grn_drainage_systems.php (last access: 1 March 2015), 2012.
Short summary
In Greenland, ice motion and the surface geometry depend on the friction at the bed. We use satellite measurements and modeling to determine how ice speeds and friction are related across the ice sheet. The relationships indicate that ice flowing over bed bumps sets the friction across most of the ice sheet's on-land regions. This result helps simplify and improve our understanding of how ice motion will change in the future.
In Greenland, ice motion and the surface geometry depend on the friction at the bed. We use...