Articles | Volume 11, issue 6
https://doi.org/10.5194/tc-11-2773-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-11-2773-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Satellite-derived submarine melt rates and mass balance (2011–2015) for Greenland's largest remaining ice tongues
MIT-WHOI Joint Program in Oceanography/Applied Ocean Science and Engineering, Cambridge, Massachusetts, USA
Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA
Fiammetta Straneo
Physical Oceanography Department, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA
now at: Scripps Institution of Oceanography, UCSD, La Jolla, CA, USA
Patrick Heimbach
Jackson School of Geosciences and Institute for Computational Engineering and Sciences, University of Texas at Austin, Austin, Texas, USA
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64 citations as recorded by crossref.
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- Supraglacial lake expansion, intensified lake drainage frequency, and first observation of coupled lake drainage, during 1985–2020 at Ryder Glacier, Northern Greenland J. Otto et al. 10.3389/feart.2022.978137
- Direct measurement of warm Atlantic Intermediate Water close to the grounding line of Nioghalvfjerdsfjorden (79° N) Glacier, northeast Greenland M. Bentley et al. 10.5194/tc-17-1821-2023
- Atmospheric blocking slows ocean-driven melting of Greenland’s largest glacier tongue R. McPherson et al. 10.1126/science.ado5008
- Basal melt rates and ocean circulation under the Ryder Glacier ice tongue and their response to climate warming: a high-resolution modelling study J. Wiskandt et al. 10.5194/tc-17-2755-2023
- Extreme melting at Greenland's largest floating ice tongue O. Zeising et al. 10.5194/tc-18-1333-2024
- Quantifying Ice‐Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ S. Krisch et al. 10.1029/2022GL100296
- Simulating the Holocene deglaciation across a marine-terminating portion of southwestern Greenland in response to marine and atmospheric forcings J. Cuzzone et al. 10.5194/tc-16-2355-2022
- Present day Jakobshavn Isbræ (West Greenland) close to the Holocene minimum extent K. Kajanto et al. 10.1016/j.quascirev.2020.106492
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- Impact of the Nares Strait sea ice arches on the long-term stability of the Petermann Glacier ice shelf A. Prakash et al. 10.5194/tc-17-5255-2023
- Impact of millennial-scale oceanic variability on the Greenland ice-sheet evolution throughout the last glacial period I. Tabone et al. 10.5194/cp-15-593-2019
- Rapid Basal Channel Growth Beneath Greenland's Longest Floating Ice Shelf A. Narkevic et al. 10.1029/2023GL103226
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- Bathymetry constrains ocean heat supply to Greenland’s largest glacier tongue J. Schaffer et al. 10.1038/s41561-019-0529-x
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- Future Evolution of Greenland's Marine‐Terminating Outlet Glaciers G. Catania et al. 10.1029/2018JF004873
- Ocean-driven millennial-scale variability of the Eurasian ice sheet during the last glacial period simulated with a hybrid ice-sheet–shelf model J. Alvarez-Solas et al. 10.5194/cp-15-957-2019
- The Relationship Between Submarine Melt and Subglacial Discharge From Observations at a Tidewater Glacier R. Jackson et al. 10.1029/2021JC018204
- Pervasive ice sheet mass loss reflects competing ocean and atmosphere processes B. Smith et al. 10.1126/science.aaz5845
- Mapping Basal Melt Under the Shackleton Ice Shelf, East Antarctica, From CryoSat-2 Radar Altimetry Q. Liang et al. 10.1109/JSTARS.2021.3077359
- Velocity response of Petermann Glacier, northwest Greenland, to past and future calving events E. Hill et al. 10.5194/tc-12-3907-2018
- Petermann ice shelf may not recover after a future breakup H. Åkesson et al. 10.1038/s41467-022-29529-5
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- Grounding-line retreat of Milne Glacier, Ellesmere Island, Canada over 1966–2023 from satellite, airborne, and ground radar data Y. Antropova et al. 10.1016/j.rse.2024.114478
- High‐Resolution Simulations of the Plume Dynamics in an Idealized 79°N Glacier Cavity Using Adaptive Vertical Coordinates M. Reinert et al. 10.1029/2023MS003721
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- Impact of paleoclimate on present and future evolution of the Greenland Ice Sheet H. Yang et al. 10.1371/journal.pone.0259816
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- Ocean melting of the Zachariae Isstrøm and Nioghalvfjerdsfjorden glaciers, northeast Greenland L. An et al. 10.1073/pnas.2015483118
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- Ryder Glacier in northwest Greenland is shielded from warm Atlantic water by a bathymetric sill M. Jakobsson et al. 10.1038/s43247-020-00043-0
- Melt rates in the kilometer-size grounding zone of Petermann Glacier, Greenland, before and during a retreat E. Ciracì et al. 10.1073/pnas.2220924120
- Ocean Circulation and Variability Beneath Nioghalvfjerdsbræ (79 North Glacier) Ice Tongue M. Lindeman et al. 10.1029/2020JC016091
- Detecting high spatial variability of ice shelf basal mass balance, Roi Baudouin Ice Shelf, Antarctica S. Berger et al. 10.5194/tc-11-2675-2017
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62 citations as recorded by crossref.
- Heat stored in the Earth system 1960–2020: where does the energy go? K. von Schuckmann et al. 10.5194/essd-15-1675-2023
- Hydraulic suppression of basal glacier melt in sill fjords J. Nilsson et al. 10.5194/tc-17-2455-2023
- Ocean Variability at Greenland's Largest Glacier Tongue Linked to Continental Shelf Circulation L. von Albedyll et al. 10.1029/2020JC017080
- Supraglacial lake expansion, intensified lake drainage frequency, and first observation of coupled lake drainage, during 1985–2020 at Ryder Glacier, Northern Greenland J. Otto et al. 10.3389/feart.2022.978137
- Direct measurement of warm Atlantic Intermediate Water close to the grounding line of Nioghalvfjerdsfjorden (79° N) Glacier, northeast Greenland M. Bentley et al. 10.5194/tc-17-1821-2023
- Atmospheric blocking slows ocean-driven melting of Greenland’s largest glacier tongue R. McPherson et al. 10.1126/science.ado5008
- Basal melt rates and ocean circulation under the Ryder Glacier ice tongue and their response to climate warming: a high-resolution modelling study J. Wiskandt et al. 10.5194/tc-17-2755-2023
- Extreme melting at Greenland's largest floating ice tongue O. Zeising et al. 10.5194/tc-18-1333-2024
- Quantifying Ice‐Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ S. Krisch et al. 10.1029/2022GL100296
- Simulating the Holocene deglaciation across a marine-terminating portion of southwestern Greenland in response to marine and atmospheric forcings J. Cuzzone et al. 10.5194/tc-16-2355-2022
- Present day Jakobshavn Isbræ (West Greenland) close to the Holocene minimum extent K. Kajanto et al. 10.1016/j.quascirev.2020.106492
- Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05) V. Arnone et al. 10.1016/j.scitotenv.2023.168162
- Impact of the Nares Strait sea ice arches on the long-term stability of the Petermann Glacier ice shelf A. Prakash et al. 10.5194/tc-17-5255-2023
- Impact of millennial-scale oceanic variability on the Greenland ice-sheet evolution throughout the last glacial period I. Tabone et al. 10.5194/cp-15-593-2019
- Rapid Basal Channel Growth Beneath Greenland's Longest Floating Ice Shelf A. Narkevic et al. 10.1029/2023GL103226
- Global environmental consequences of twenty-first-century ice-sheet melt N. Golledge et al. 10.1038/s41586-019-0889-9
- Bathymetry constrains ocean heat supply to Greenland’s largest glacier tongue J. Schaffer et al. 10.1038/s41561-019-0529-x
- Impacts of glacier and sea ice melt on methane pathways on the Northeast Greenland shelf J. Verdugo et al. 10.1016/j.csr.2022.104752
- Ongoing grounding line retreat and fracturing initiated at the Petermann Glacier ice shelf, Greenland, after 2016 R. Millan et al. 10.5194/tc-16-3021-2022
- Future Evolution of Greenland's Marine‐Terminating Outlet Glaciers G. Catania et al. 10.1029/2018JF004873
- Ocean-driven millennial-scale variability of the Eurasian ice sheet during the last glacial period simulated with a hybrid ice-sheet–shelf model J. Alvarez-Solas et al. 10.5194/cp-15-957-2019
- The Relationship Between Submarine Melt and Subglacial Discharge From Observations at a Tidewater Glacier R. Jackson et al. 10.1029/2021JC018204
- Pervasive ice sheet mass loss reflects competing ocean and atmosphere processes B. Smith et al. 10.1126/science.aaz5845
- Mapping Basal Melt Under the Shackleton Ice Shelf, East Antarctica, From CryoSat-2 Radar Altimetry Q. Liang et al. 10.1109/JSTARS.2021.3077359
- Velocity response of Petermann Glacier, northwest Greenland, to past and future calving events E. Hill et al. 10.5194/tc-12-3907-2018
- Petermann ice shelf may not recover after a future breakup H. Åkesson et al. 10.1038/s41467-022-29529-5
- Sensitivity to forecast surface mass balance outweighs sensitivity to basal sliding descriptions for 21st century mass loss from three major Greenland outlet glaciers J. Carr et al. 10.5194/tc-18-2719-2024
- Grounding-line retreat of Milne Glacier, Ellesmere Island, Canada over 1966–2023 from satellite, airborne, and ground radar data Y. Antropova et al. 10.1016/j.rse.2024.114478
- High‐Resolution Simulations of the Plume Dynamics in an Idealized 79°N Glacier Cavity Using Adaptive Vertical Coordinates M. Reinert et al. 10.1029/2023MS003721
- Properties and dynamics of mesoscale eddies in Fram Strait from a comparison between two high-resolution ocean–sea ice models C. Wekerle et al. 10.5194/os-16-1225-2020
- Arctic – Atlantic Exchange of the Dissolved Micronutrients Iron, Manganese, Cobalt, Nickel, Copper and Zinc With a Focus on Fram Strait S. Krisch et al. 10.1029/2021GB007191
- Shifts of the Recirculation Pathways in Central Fram Strait Drive Atlantic Intermediate Water Variability on Northeast Greenland Shelf R. McPherson et al. 10.1029/2023JC019915
- Sensitivity of Greenland ice sheet projections to spatial resolution in higher-order simulations: the Alfred Wegener Institute (AWI) contribution to ISMIP6 Greenland using the Ice-sheet and Sea-level System Model (ISSM) M. Rückamp et al. 10.5194/tc-14-3309-2020
- Calving Induced Speedup of Petermann Glacier M. Rückamp et al. 10.1029/2018JF004775
- Tidal Modulation of Buoyant Flow and Basal Melt Beneath Petermann Gletscher Ice Shelf, Greenland P. Washam et al. 10.1029/2020JC016427
- Glacier-specific factors drive differing seasonal and interannual dynamics of Nunatakassaap Sermia and Illullip Sermia, Greenland J. Carr et al. 10.1080/15230430.2023.2186456
- Twenty-first century response of Petermann Glacier, northwest Greenland to ice shelf loss E. Hill et al. 10.1017/jog.2020.97
- Grounding Line Retreat of Denman Glacier, East Antarctica, Measured With COSMO‐SkyMed Radar Interferometry Data V. Brancato et al. 10.1029/2019GL086291
- The sensitivity of the Greenland Ice Sheet to glacial–interglacial oceanic forcing I. Tabone et al. 10.5194/cp-14-455-2018
- Large spatial variations in the flux balance along the front of a Greenland tidewater glacier T. Wagner et al. 10.5194/tc-13-911-2019
- A nested high-resolution unstructured grid 3-D ocean-sea ice-ice shelf setup for numerical investigations of the Petermann ice shelf and fjord A. Prakash et al. 10.1016/j.mex.2022.101668
- Submarine Meltwater From Nioghalvfjerdsbræ (79 North Glacier), Northeast Greenland O. Huhn et al. 10.1029/2021JC017224
- Estimating Spring Terminus Submarine Melt Rates at a Greenlandic Tidewater Glacier Using Satellite Imagery A. Moyer et al. 10.3389/feart.2017.00107
- Summer surface melt thins Petermann Gletscher Ice Shelf by enhancing channelized basal melt P. WASHAM et al. 10.1017/jog.2019.43
- Impact of paleoclimate on present and future evolution of the Greenland Ice Sheet H. Yang et al. 10.1371/journal.pone.0259816
- Future Projections of Petermann Glacier Under Ocean Warming Depend Strongly on Friction Law H. Åkesson et al. 10.1029/2020JF005921
- High-resolution mascon solutions reveal glacier-scale mass changes over the Greenland Ice Sheet from 2002 to 2022 W. Wang et al. 10.1093/gji/ggad439
- The Case for a Sustained Greenland Ice Sheet-Ocean Observing System (GrIOOS) F. Straneo et al. 10.3389/fmars.2019.00138
- Submarine melt as a potential trigger of the North East Greenland Ice Stream margin retreat during Marine Isotope Stage 3 I. Tabone et al. 10.5194/tc-13-1911-2019
- Heat stored in the Earth system: where does the energy go? K. von Schuckmann et al. 10.5194/essd-12-2013-2020
- Ice shelf basal melt rates from a high-resolution digital elevation model (DEM) record for Pine Island Glacier, Antarctica D. Shean et al. 10.5194/tc-13-2633-2019
- Past and future ocean warming L. Cheng et al. 10.1038/s43017-022-00345-1
- Atlantic Water warming increases melt below Northeast Greenland’s last floating ice tongue C. Wekerle et al. 10.1038/s41467-024-45650-z
- Ocean melting of the Zachariae Isstrøm and Nioghalvfjerdsfjorden glaciers, northeast Greenland L. An et al. 10.1073/pnas.2015483118
- Mass Balances of the Antarctic and Greenland Ice Sheets Monitored from Space I. Otosaka et al. 10.1007/s10712-023-09795-8
- Precursor of disintegration of Greenland's largest floating ice tongue A. Humbert et al. 10.5194/tc-17-2851-2023
- The effect of overshooting 1.5 °C global warming on the mass loss of the Greenland ice sheet M. Rückamp et al. 10.5194/esd-9-1169-2018
- A candle burning from both ends H. Seroussi & C. Meyer 10.1038/s41558-022-01357-x
- Calving at Ryder Glacier, Northern Greenland F. Holmes et al. 10.1029/2020JF005872
- Ryder Glacier in northwest Greenland is shielded from warm Atlantic water by a bathymetric sill M. Jakobsson et al. 10.1038/s43247-020-00043-0
- Melt rates in the kilometer-size grounding zone of Petermann Glacier, Greenland, before and during a retreat E. Ciracì et al. 10.1073/pnas.2220924120
- Ocean Circulation and Variability Beneath Nioghalvfjerdsbræ (79 North Glacier) Ice Tongue M. Lindeman et al. 10.1029/2020JC016091
Latest update: 20 Nov 2024
Short summary
We estimate submarine melt rates from ice tongues in northern Greenland using WorldView satellite imagery. At Ryder Glacier, melt is strongly concentrated around regions where subglacier channels likely enter the fjord. At the 79 North Glacier, we find a large volume imbalance in which melting removes a greater quantity of ice than is replaced by inflow over the grounding line. This leads us to suggest that a reduction in the spatial extent of the ice tongue is possible over the coming decade.
We estimate submarine melt rates from ice tongues in northern Greenland using WorldView...