Articles | Volume 12, issue 10
https://doi.org/10.5194/tc-12-3287-2018
© 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-12-3287-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Brief communication: Recent changes in summer Greenland blocking captured by none of the CMIP5 models
Edward Hanna
CORRESPONDING AUTHOR
School of Geography and Lincoln Centre for Water and Planetary
Health, University of Lincoln, Lincoln, UK
Xavier Fettweis
Laboratory of
Climatology, Department of Geography, University of Liège, Liège,
Belgium
Richard J. Hall
School of Geography and Lincoln Centre for Water and Planetary
Health, University of Lincoln, Lincoln, UK
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2 citations as recorded by crossref.
- Atmospheric Blocking Drives Recent Albedo Change Across the Western Greenland Ice Sheet Percolation Zone G. Lewis et al. 10.1029/2021GL092814
- Brief communication: Impact of the recent atmospheric circulation change in summer on the future surface mass balance of the Greenland Ice Sheet A. Delhasse et al. 10.5194/tc-12-3409-2018
Discussed (final revised paper)
Latest update: 10 Dec 2024
Short summary
The latest/recent generations of global climate models do not simulate the recent (last 30 years) increase in atmospheric high pressure over Greenland in summer but rather projects decreasing pressure.
This difference between climate models and observations raises serious questions about the ability of the models to accurately represent future changes in Greenland climate and ice-sheet mass balance. There are also likely effects on climate predictions downstream, e.g. over Europe.
The latest/recent generations of global climate models do not simulate the recent (last 30...