Sensitivity of ice loss to uncertainty in flow law parameters in an idealized one-dimensional geometry
<p>Acceleration of the flow of ice drives mass losses in both the Antarctic and the Greenland Ice Sheet. The projections of possible future sea-level rise rely on numerical ice-sheet models, which solve the physics of ice flow, melt, and calving. While major advancements have been made by the...
Main Authors: | M. Zeitz, A. Levermann, R. Winkelmann |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2020-10-01
|
Series: | The Cryosphere |
Online Access: | https://tc.copernicus.org/articles/14/3537/2020/tc-14-3537-2020.pdf |
Similar Items
-
Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) – Part 2: Parameter ensemble analysis
by: T. Albrecht, et al.
Published: (2020-02-01) -
Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) – Part 1: Boundary conditions and climatic forcing
by: T. Albrecht, et al.
Published: (2020-02-01) -
A simple equation for the melt elevation feedback of ice sheets
by: A. Levermann, et al.
Published: (2016-08-01) -
The role of history and strength of the oceanic forcing in sea level projections from Antarctica with the Parallel Ice Sheet Model
by: R. Reese, et al.
Published: (2020-09-01) -
Similitude of ice dynamics against scaling of geometry and physical parameters
by: J. Feldmann, et al.
Published: (2016-08-01)