Land-ice modeling for sea-level prediction

There has been major progress in ice sheet modeling since IPCC AR4. We will soon have efficient higherorder ice sheet models that can run at ",1 km resolution for entire ice sheets, either standalone or coupled to GeMs. These models should significantly reduce uncertainties in sea-level predict...

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Bibliographic Details
Main Author: Lipscomb, William H
Language:unknown
Published: 2021
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1172858
https://www.osti.gov/biblio/1172858
https://doi.org/10.2172/1172858
Description
Summary:There has been major progress in ice sheet modeling since IPCC AR4. We will soon have efficient higherorder ice sheet models that can run at ",1 km resolution for entire ice sheets, either standalone or coupled to GeMs. These models should significantly reduce uncertainties in sea-level predictions. However, the least certain and potentially greatest contributions to 21st century sea-level rise may come from ice-ocean interactions, especially in West Antarctica. This is a coupled modeling problem that requires collaboration among ice, ocean and atmosphere modelers.