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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 3
Geosci. Model Dev., 9, 1087-1109, 2016
https://doi.org/10.5194/gmd-9-1087-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Geosci. Model Dev., 9, 1087-1109, 2016
https://doi.org/10.5194/gmd-9-1087-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Model description paper 18 Mar 2016

Model description paper | 18 Mar 2016

ISSM-SESAW v1.0: mesh-based computation of gravitationally consistent sea-level and geodetic signatures caused by cryosphere and climate driven mass change

Surendra Adhikari et al.
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A, G., Wahr, J., and Zhong, S.: Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada, Geophys. J. Int., 192, 557–572, https://doi.org/10.1093/gji/ggs030, 2013.
Adhikari, S., Ivins, E. R., Larour, E., Seroussi, H., Morlighem, M., and Nowicki, S.: Future Antarctic bed topography and its implications for ice sheet dynamics, Solid Earth, 5, 569–584, https://doi.org/10.5194/se-5-569-2014, 2014.
Bamber, J. L. and Aspinall, W. P.: An expert judgement assessment of future sea level rise from the ice sheets, Nature Clim. Change, 3, 424–427, 2013.
Bettadpur, S.: GRACE 327-742, UTCSR Level-2 Processing Standards Document for Level-2 Product Release 0005, Tech. rep., The University of Texas at Austin, Texas, USA, 2012.
Blewitt, G.: Self-consistency in reference frames, geocenter definition, and surface loading of the solid Earth, J. Geophys. Res., 108, B22103, https://doi.org/10.1029/2002JB002082, 2003.
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We present a numerically accurate, computationally efficient, (km-scale) high-resolution model for gravitationally consistent relative sea level that, unlike contemporary state-of-the-art models, operates efficiently on an unstructured mesh. The model is useful for earth system modeling and space geodesy. A straightforward and computationally less burdensome coupling to a dynamical ice-sheet model, for example, allows a refined and realistic simulation of fast-flowing outlet glaciers.
We present a numerically accurate, computationally efficient, (km-scale) high-resolution model...
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