Articles | Volume 12, issue 11
https://doi.org/10.5194/tc-12-3409-2018
© Author(s) 2018. 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-12-3409-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Brief communication: Impact of the recent atmospheric circulation change in summer on the future surface mass balance of the Greenland Ice Sheet
Alison Delhasse
CORRESPONDING AUTHOR
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Xavier Fettweis
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Christoph Kittel
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Charles Amory
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Cécile Agosta
Laboratory of Climatology, Department of Geography, University of Liège, Liège, Belgium
Laboratoire des Sciences du Climat et de l'Environnement, Gif-sur-Yvette, France
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- Brief communication: CMIP6 does not suggest any atmospheric blocking increase in summer over Greenland by 2100 A. Delhasse et al. 10.1002/joc.6977
- Cloud microphysics and circulation anomalies control differences in future Greenland melt S. Hofer et al. 10.1038/s41558-019-0507-8
- Spatially Heterogeneous Effects of Atmospheric Circulation on Greenland Ice Sheet Melting H. Wang et al. 10.3390/atmos15010057
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- Effects of extreme melt events on ice flow and sea level rise of the Greenland Ice Sheet J. Beckmann & R. Winkelmann 10.5194/tc-17-3083-2023
- Atmospheric drivers of melt-related ice speed-up events on the Russell Glacier in southwest Greenland T. Schmid et al. 10.5194/tc-17-3933-2023
- Greenland surface air temperature changes from 1981 to 2019 and implications for ice‐sheet melt and mass‐balance change E. Hanna et al. 10.1002/joc.6771
- Changes in elevation and mass of Arctic glaciers and ice caps, 2010–2017 P. Tepes et al. 10.1016/j.rse.2021.112481
- Diverse supraglacial drainage patterns on the Devon ice Cap, Arctic Canada Y. Lu et al. 10.1080/17445647.2020.1838353
- Discrepancies between observations and climate models of large-scale wind-driven Greenland melt influence sea-level rise projections D. Topál et al. 10.1038/s41467-022-34414-2
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- Brief communication: Evaluation of the near-surface climate in ERA5 over the Greenland Ice Sheet A. Delhasse et al. 10.5194/tc-14-957-2020
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- Atmospheric circulation-constrained model sensitivity recalibrates Arctic climate projections D. Topál & Q. Ding 10.1038/s41558-023-01698-1
- Summer atmospheric circulation over Greenland in response to Arctic amplification and diminished spring snow cover J. Preece et al. 10.1038/s41467-023-39466-6
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- Accumulation rates (2009–2017) in Southeast Greenland derived from airborne snow radar and comparison with regional climate models L. Montgomery et al. 10.1017/aog.2020.8
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- GrSMBMIP: intercomparison of the modelled 1980–2012 surface mass balance over the Greenland Ice Sheet X. Fettweis et al. 10.5194/tc-14-3935-2020
- Critical slowing down suggests that the western Greenland Ice Sheet is close to a tipping point N. Boers & M. Rypdal 10.1073/pnas.2024192118
- Brief communication: CESM2 climate forcing (1950–2014) yields realistic Greenland ice sheet surface mass balance B. Noël et al. 10.5194/tc-14-1425-2020
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- Strong Summer Atmospheric Rivers Trigger Greenland Ice Sheet Melt through Spatially Varying Surface Energy Balance and Cloud Regimes K. Mattingly et al. 10.1175/JCLI-D-19-0835.1
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- Atmospheric Blocking Drives Recent Albedo Change Across the Western Greenland Ice Sheet Percolation Zone G. Lewis et al. 10.1029/2021GL092814
- North Atlantic Footprint of Summer Greenland Ice Sheet Melting on Interannual to Interdecadal Time Scales: A Greenland Blocking Perspective H. Wang & D. Luo 10.1175/JCLI-D-21-0382.1
- Impacts of Greenland Block Location on Clouds and Surface Energy Fluxes Over the Greenland Ice Sheet J. Ward et al. 10.1029/2020JD033172
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Short summary
Since the 2000s, an atmospheric circulation change (CC) gauged by a negative summer shift in the North Atlantic Oscillation has been observed, enhancing surface melt over the Greenland Ice Sheet (GrIS). Future GrIS surface mass balance (SMB) projections are based on global climate models that do not represent this CC. The model MAR has been used to show that previous estimates of these projections could have been significantly overestimated if this current circulation pattern persists.
Since the 2000s, an atmospheric circulation change (CC) gauged by a negative summer shift in the...