Reference : Century-scale simulations of the response of the West Antarctic Ice Sheet to a warmin...
Scientific journals : Article
Physical, chemical, mathematical & earth Sciences : Earth sciences & physical geography
http://hdl.handle.net/2268/182856
Century-scale simulations of the response of the West Antarctic Ice Sheet to a warming climate
English
Cornford, S.L. [> >]
Martin, D.F. [> >]
Payne, A.J. [> >]
Ng, E.G. [> >]
Le Brocq, A.M. [> >]
Gladstone, R.M. [> >]
Edwards, T.L. [> >]
Shannon, S.R. [> >]
Agosta, Cécile mailto [Université de Liège > Département de géographie > Climatologie et Topoclimatologie >]
van den Broeke, M.R. [> >]
Hellmer, H. [> >]
Krinner, G. [> >]
Ligtenberg, S.R.M. [> >]
Timmermann, R. [> >]
Vaughan, D.G. [> >]
18-Aug-2015
Cryosphere
Copernicus
9
1579-1600
Yes (verified by ORBi)
International
1994-0416
1994-0424
Katlenberg-Lindau
Germany
[en] Antarctica ; ice-sheet ; warming ; climate change
[en] We use the BISICLES adaptive mesh ice sheet model to carry out one, two, and three century simulations of the fast-flowing ice streams of the West Antarctic Ice Sheet, deploying sub-kilometer resolution around the grounding line since coarser resolution results in substantial underestimation of the response. Each of the simulations begins with a geometry and velocity close to present-day observations, and evolves according to variation in meteoric ice accumulation rates and oceanic ice shelf melt rates. Future changes in accumulation and melt rates range from no change, through anomalies computed by atmosphere and ocean models driven by the E1 and A1B emissions scenarios, to spatially uniform melt rate anomalies that remove most of the ice shelves over a few centuries. We find that variation in the resulting ice dynamics is dominated by the choice of initial conditions and ice shelf melt rate and mesh resolution, although ice accumulation affects the net change in volume above flotation to a similar degree. Given sufficient melt rates, we compute grounding line retreat over hundreds of kilometers in every major ice stream, but the ocean models do not predict such melt rates outside of the Amundsen Sea Embayment until after 2100. Within the Amundsen Sea Embayment the largest single source of variability is the onset of sustained retreat in Thwaites Glacier, which can triple the rate of eustatic sea level rise.
Researchers ; Professionals ; Students
http://hdl.handle.net/2268/182856
10.5194/tc-9-1579-2015
http://www.the-cryosphere.net/9/1579/2015/

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