Bitte benutzen Sie diesen Identifier, um auf die Ressource zu verweisen: https://oar.tib.eu/jspui/handle/123456789/685
Dateien zu dieser Publikation:
Datei GrößeFormat 
tc-9-631-2015.pdf4.02 MBAdobe PDFAnzeigen/Öffnen
Titel: Simulating the Greenland ice sheet under present-day and palaeo constraints including a new discharge parameterization
Autor(en): Calov, R.Robinson, A.Perrette, M.Ganopolski, A.
Verlagsversion: https://doi.org/10.5194/tc-9-631-2015
Erscheinungsjahr: 2015
Publiziert in: The Cryosphere, Volume 9, Issue 1, Page 179-196
Verlag: München : European Geopyhsical Union
Abstract: In this paper, we propose a new sub-grid scale parameterization for the ice discharge into the ocean through outlet glaciers and inspect the role of different observational and palaeo constraints for the choice of an optimal set of model parameters. This parameterization was introduced into the polythermal ice-sheet model SICOPOLIS, which is coupled to the regional climate model of intermediate complexity REMBO. Using the coupled model, we performed large ensemble simulations over the last two glacial cycles by varying two major parameters: a melt parameter in the surface melt scheme of REMBO and a discharge scaling parameter in our parameterization of ice discharge. Our empirical constraints are the present-day Greenland ice sheet surface elevation, the surface mass balance partition (ratio between total ice discharge and total precipitation) and the Eemian interglacial elevation drop relative to present day in the vicinity of the NEEM ice core. We show that the ice discharge parameterization enables us to simulate both the correct ice-sheet shape and mass balance partition at the same time without explicitly resolving the Greenland outlet glaciers. For model verification, we compare the simulated total and sectoral ice discharge with other estimates. For the model versions that are consistent with the range of observational and palaeo constraints, our simulated Greenland ice sheet contribution to Eemian sea-level rise relative to present-day amounts to 1.4 m on average (in the range of 0.6 and 2.5 m).
Schlagwörter: Discharge; glacial hydrology; ice flow; ice sheet; mass balance; melting; parameterization; sea level change
DDC: 550
Lizenz: CC BY 3.0 Unported
Link zur Lizenz: https://creativecommons.org/licenses/by/3.0/
Enthalten in den Sammlungen:Geowissenschaften

Zur Langanzeige


Diese Publikatione wurde unter der folgenden Lizenz verouml;ffentlicht: Creative-Commons-Lizenz Creative Commons