Assessment of errors and uncertainty patterns in GIA modeling

During the last decade many efforts have been devoted to the assessment of global sea level rise and to the determination of the mass balance of continental ice sheets. In this context, the important role of glacial-isostatic adjustment (GIA) has been clearly recognized. Yet, in many cases only one...

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Main Authors: Barletta, Valentina Roberta, Spada, G.
Format: Conference Object
Language:English
Published: 2012
Subjects:
Online Access:https://orbit.dtu.dk/en/publications/685c99c6-14f5-455c-9af2-e9c8fb5e6e5b
https://backend.orbit.dtu.dk/ws/files/9770936/c.pdf
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spelling ftdtupubl:oai:pure.atira.dk:publications/685c99c6-14f5-455c-9af2-e9c8fb5e6e5b 2023-05-15T13:54:38+02:00 Assessment of errors and uncertainty patterns in GIA modeling Barletta, Valentina Roberta Spada, G. 2012 application/pdf https://orbit.dtu.dk/en/publications/685c99c6-14f5-455c-9af2-e9c8fb5e6e5b https://backend.orbit.dtu.dk/ws/files/9770936/c.pdf eng eng info:eu-repo/semantics/openAccess Barletta , V R & Spada , G 2012 , ' Assessment of errors and uncertainty patterns in GIA modeling ' , Geophysical Research Abstracts , vol. 14 , pp. EGU2012-9717 . conferenceObject 2012 ftdtupubl 2022-08-14T08:12:19Z During the last decade many efforts have been devoted to the assessment of global sea level rise and to the determination of the mass balance of continental ice sheets. In this context, the important role of glacial-isostatic adjustment (GIA) has been clearly recognized. Yet, in many cases only one "preferred" GIA model has been used, without any consideration of the possible errors involved. Lacking a rigorous assessment of systematic errors in GIA modeling, the reliability of the results is uncertain. GIA sensitivity and uncertainties associated with the viscosity models have been explored in the literature. However, at least two major sources of errors remain. The first is associated with the ice models, spatial distribution of ice and history of melting (this is especially the case of Antarctica), the second with the numerical implementation of model features relevant to sea level modeling, such as time-evolving shorelines and paleo coastlines. In this study we quantify these uncertainties and their propagation in GIA response using a Monte Carlo approach to obtain spatio-temporal patterns of GIA errors. A direct application is the error estimates in ice mass balance in Antarctica and Greenland due to GIA. GIA errors are also important in the far field of previously glaciated areas and in the time evolution of global indicators. In this regard we also account for other possible errors sources which can impact global indicators like the sea level history related to GIA. Conference Object Antarc* Antarctica Greenland Technical University of Denmark: DTU Orbit Greenland
institution Open Polar
collection Technical University of Denmark: DTU Orbit
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language English
description During the last decade many efforts have been devoted to the assessment of global sea level rise and to the determination of the mass balance of continental ice sheets. In this context, the important role of glacial-isostatic adjustment (GIA) has been clearly recognized. Yet, in many cases only one "preferred" GIA model has been used, without any consideration of the possible errors involved. Lacking a rigorous assessment of systematic errors in GIA modeling, the reliability of the results is uncertain. GIA sensitivity and uncertainties associated with the viscosity models have been explored in the literature. However, at least two major sources of errors remain. The first is associated with the ice models, spatial distribution of ice and history of melting (this is especially the case of Antarctica), the second with the numerical implementation of model features relevant to sea level modeling, such as time-evolving shorelines and paleo coastlines. In this study we quantify these uncertainties and their propagation in GIA response using a Monte Carlo approach to obtain spatio-temporal patterns of GIA errors. A direct application is the error estimates in ice mass balance in Antarctica and Greenland due to GIA. GIA errors are also important in the far field of previously glaciated areas and in the time evolution of global indicators. In this regard we also account for other possible errors sources which can impact global indicators like the sea level history related to GIA.
format Conference Object
author Barletta, Valentina Roberta
Spada, G.
spellingShingle Barletta, Valentina Roberta
Spada, G.
Assessment of errors and uncertainty patterns in GIA modeling
author_facet Barletta, Valentina Roberta
Spada, G.
author_sort Barletta, Valentina Roberta
title Assessment of errors and uncertainty patterns in GIA modeling
title_short Assessment of errors and uncertainty patterns in GIA modeling
title_full Assessment of errors and uncertainty patterns in GIA modeling
title_fullStr Assessment of errors and uncertainty patterns in GIA modeling
title_full_unstemmed Assessment of errors and uncertainty patterns in GIA modeling
title_sort assessment of errors and uncertainty patterns in gia modeling
publishDate 2012
url https://orbit.dtu.dk/en/publications/685c99c6-14f5-455c-9af2-e9c8fb5e6e5b
https://backend.orbit.dtu.dk/ws/files/9770936/c.pdf
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
genre_facet Antarc*
Antarctica
Greenland
op_source Barletta , V R & Spada , G 2012 , ' Assessment of errors and uncertainty patterns in GIA modeling ' , Geophysical Research Abstracts , vol. 14 , pp. EGU2012-9717 .
op_rights info:eu-repo/semantics/openAccess
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