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New method relates Greenland ice sheet changes to sea-level rise

Date:
April 14, 2015
Source:
Department of Energy, Office of Science
Summary:
Early schemes to model the Greenland and Antarctic ice sheets and their impact on sea levels failed to accurately account for changes caused by snowfall and snow melt. These changes depend on ice sheet elevation and region. Researchers developed a new method that includes the effects of elevation and region.
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Climate models are not yet able to include full models of the Greenland and Antarctic ice sheets and to dynamically simulate how ice sheet changes influence sea level. Early schemes failed to accurately account for both mass increase due to snowfall and mass loss due to snow melt. These increases and losses depend on ice sheet elevation and region. A new method that includes the effects of elevation and region was developed using a detailed regional model of the Greenland ice sheet.

Using the new scheme on different models with different climate warming conditions, developed jointly by several ice sheet research groups, including two funded by the U.S. Department of Energy, improves the ability of the models to assess sea-level rise. The results provide insights to guide ongoing development of fully dynamic coupled ice sheet models.

The team used the new scheme in five ice sheet models and forced them with climate warming conditions taken from two different climate models. Including the elevation effects in the model increases the estimated sea-level rise by a small but significant amount (5% enhancement of melt by 2100 and 10% by 2200 for a climate warming scenario). By 2100, the choice of driving climate model conditions dominates the uncertainty, but by 2200, the uncertainty in the ice sheet model and the elevation scheme are larger.

Research from Edwards et al. 2014a was funded by the ice2sea programme from the European Union (EU) 7th Framework Programme (grant number 226375; ice2sea contribution number 120). Additional support provided by the Advanced Scientific Computing Research and Biological and Environmental Research programs within the U.S. Department of Energy's Office of Science, along with the Center for Remote Sensing of Ice Sheets at the University of Kansas through National Science Foundation grant ANT-0424589.

Research from Edwards et al. 2014b was supported by funding from the ice2sea programme from the EU 7th Framework Programme (grant number 226375; ice2sea contribution number 151). Elmer/Ice simulations were performed using high-performance computing resources from GENCI-CINES (grant 2011016066) and from the Service Commun de Calcul Intensif de l'Observatoire de Grenoble (SCCI).


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Journal References:

  1. T. L. Edwards, X. Fettweis, O. Gagliardini, F. Gillet-Chaulet, H. Goelzer, J. M. Gregory, M. Hoffman, P. Huybrechts, A. J. Payne, M. Perego, S. Price, A. Quiquet, C. Ritz. Probabilistic parameterisation of the surface mass balance–elevation feedback in regional climate model simulations of the Greenland ice sheet. The Cryosphere, 2014; 8 (1): 181 DOI: 10.5194/tc-8-181-2014
  2. T. L. Edwards, X. Fettweis, O. Gagliardini, F. Gillet-Chaulet, H. Goelzer, J. M. Gregory, M. Hoffman, P. Huybrechts, A. J. Payne, M. Perego, S. Price, A. Quiquet, C. Ritz. Effect of uncertainty in surface mass balance–elevation feedback on projections of the future sea level contribution of the Greenland ice sheet. The Cryosphere, 2014; 8 (1): 195 DOI: 10.5194/tc-8-195-2014

Cite This Page:

Department of Energy, Office of Science. "New method relates Greenland ice sheet changes to sea-level rise." ScienceDaily. ScienceDaily, 14 April 2015. <www.sciencedaily.com/releases/2015/04/150414093550.htm>.
Department of Energy, Office of Science. (2015, April 14). New method relates Greenland ice sheet changes to sea-level rise. ScienceDaily. Retrieved May 23, 2017 from www.sciencedaily.com/releases/2015/04/150414093550.htm
Department of Energy, Office of Science. "New method relates Greenland ice sheet changes to sea-level rise." ScienceDaily. www.sciencedaily.com/releases/2015/04/150414093550.htm (accessed May 23, 2017).

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