Long‐term projections of sea‐level rise from ice sheets

Under future climate change scenarios it is virtually certain that global mean sea level will continue to rise. But the rate at which this occurs, and the height and time at which it might stabilize, are uncertain. The largest potential contributors to sea level are the Greenland and Antarctic ice s...

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Published in:WIREs Climate Change
Main Author: Nicholas R. Golledge
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://doi.org/10.1002/wcc.634
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spelling ftrepec:oai:RePEc:wly:wirecc:v:11:y:2020:i:2:n:e634 2023-05-15T13:56:33+02:00 Long‐term projections of sea‐level rise from ice sheets Nicholas R. Golledge https://doi.org/10.1002/wcc.634 unknown https://doi.org/10.1002/wcc.634 article ftrepec https://doi.org/10.1002/wcc.634 2020-12-04T13:31:40Z Under future climate change scenarios it is virtually certain that global mean sea level will continue to rise. But the rate at which this occurs, and the height and time at which it might stabilize, are uncertain. The largest potential contributors to sea level are the Greenland and Antarctic ice sheets, but these may take thousands of years to fully adjust to environmental changes. Modeled projections of how these ice masses will evolve in the future are numerous, but vary both in complexity and projection timescale. Typically, there is greater agreement between models in the present century than over the next millennium. This reflects uncertainty in the physical processes that dominate ice‐sheet change and also feedbacks in the ice–atmosphere–ocean system, and how these might lead to nonlinear behavior. Satellite observations help constrain short‐term projections of ice‐sheet change but these records are still too short to capture the full ice‐sheet response. Conversely, geological records can be used to inform long‐term ice‐sheet simulations but are prone to large uncertainties, meaning that they are often unable to adequately confirm or refute the operation of particular processes. Because of these limitations there is a clear need to more accurately reconstruct sea level changes during periods of the past, to improve the spatial and temporal extent of current ice sheet observations, and to robustly attribute observed changes to driving mechanisms. Improved future projections will require models that capture a more extensive suite of physical processes than are presently incorporated, and which better quantify the associated uncertainties. This article is categorized under: Climate Models and Modeling > Knowledge Generation with Models Article in Journal/Newspaper Antarc* Antarctic Greenland Ice Sheet RePEc (Research Papers in Economics) Antarctic Greenland WIREs Climate Change 11 2
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Under future climate change scenarios it is virtually certain that global mean sea level will continue to rise. But the rate at which this occurs, and the height and time at which it might stabilize, are uncertain. The largest potential contributors to sea level are the Greenland and Antarctic ice sheets, but these may take thousands of years to fully adjust to environmental changes. Modeled projections of how these ice masses will evolve in the future are numerous, but vary both in complexity and projection timescale. Typically, there is greater agreement between models in the present century than over the next millennium. This reflects uncertainty in the physical processes that dominate ice‐sheet change and also feedbacks in the ice–atmosphere–ocean system, and how these might lead to nonlinear behavior. Satellite observations help constrain short‐term projections of ice‐sheet change but these records are still too short to capture the full ice‐sheet response. Conversely, geological records can be used to inform long‐term ice‐sheet simulations but are prone to large uncertainties, meaning that they are often unable to adequately confirm or refute the operation of particular processes. Because of these limitations there is a clear need to more accurately reconstruct sea level changes during periods of the past, to improve the spatial and temporal extent of current ice sheet observations, and to robustly attribute observed changes to driving mechanisms. Improved future projections will require models that capture a more extensive suite of physical processes than are presently incorporated, and which better quantify the associated uncertainties. This article is categorized under: Climate Models and Modeling > Knowledge Generation with Models
format Article in Journal/Newspaper
author Nicholas R. Golledge
spellingShingle Nicholas R. Golledge
Long‐term projections of sea‐level rise from ice sheets
author_facet Nicholas R. Golledge
author_sort Nicholas R. Golledge
title Long‐term projections of sea‐level rise from ice sheets
title_short Long‐term projections of sea‐level rise from ice sheets
title_full Long‐term projections of sea‐level rise from ice sheets
title_fullStr Long‐term projections of sea‐level rise from ice sheets
title_full_unstemmed Long‐term projections of sea‐level rise from ice sheets
title_sort long‐term projections of sea‐level rise from ice sheets
url https://doi.org/10.1002/wcc.634
geographic Antarctic
Greenland
geographic_facet Antarctic
Greenland
genre Antarc*
Antarctic
Greenland
Ice Sheet
genre_facet Antarc*
Antarctic
Greenland
Ice Sheet
op_relation https://doi.org/10.1002/wcc.634
op_doi https://doi.org/10.1002/wcc.634
container_title WIREs Climate Change
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container_issue 2
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