Although the net loss of ice from ice sheets to the ocean is a major contributor to historical and projected future sea-level rise, sea level does not change uniformly. The Earth responds to changes in land ice mass through a combination of adjustments to its gravitational field and rotational axis, and viscoelastic deformation of the crust and mantle, termed Glacial Isostatic Adjustment (GIA). These GIA effects induce geographically varying distribution of melt water and result in regional sea-level change that can vary from the global mean rate by 50% or more. In ISMIP6, intercomparison results were presented solely as equivalent changes to global mean sea level, and evaluation of regional sea-level effects were left to other researchers. To improve upon the status quo, in this activity we propose to integrate the production of regional sea-level projections directly into the ISMIP7 project. This task will be done by processing the ice-sheet mass change output from the ISMIP7 experiments using GIA models to produce regional sea level projections. Similar to ice-sheet modeling, there are many groups engaged in GIA and sea-level modeling with differing methodologies and models of differing complexity. In this activity we will organize an additional model intercomparison exercise to coordinate these groups to produce regional sea-level projections from the ISMIP7 ensemble. This activity will include the following tasks: (a) Preparation of ISMIP7 output for use by sea-level models, (b) Developing and testing protocols, (c) Coordination and analysis of submissions from sea-level models with different complexity and fidelity. Our primary deliverable will be a publication summarizing projections of regional sea-level change caused by future ice-sheet changes, focusing on regional variability and uncertainty at critical coastal cities and regions.
Establish protocol for bedrock adjustment in ice-sheet models
Define methodology for calculating global mean sea-level contribution from ice sheets
Provide estimates of regional sea-level change
Ice mass changes affect Earth's gravity, rotation, and crust, leading to GRD (gravitational, rotational, and deformation) effects.
Simulation Methods:
Global 3D/1D viscoelastic or elastic sea-level models
Regional (visco)elastic GIA models or ELRA
Green’s function approximation (e.g., Adhikari)
Global GIA emulators
Future Work:
Provide recommended Earth parameters (e.g., for East vs. West Antarctica)
Output bedrock deformation and geoid change separately (requires CF-compliant metadata)
Address grid interpolation issues in masked fields
ISMIP7 requires a consistent, policy-relevant way to report sea-level contributions from various ice sheet models
Volume Above Flotation (VAF) / Ocean Area has worked well in the past for its simplicity and clarity
However, this method is no longer viable due to bedrock changes and grounding line migration complexities
Uses sea-level and GIA models for more detailed, location-specific projections
GRDMIP (Gravitationally self-consistent sea-level Response to ice mass Distribution and Migration Intercomparison Project) leads regional efforts
Lead organizer: Holly Han (JPL)
Partners: ISMIP7 (future projections) and PALSEA (past reconstructions)