Hindcasting to measure ice sheet model sensitivity to initial states

Validation is a critical component of model development, yet notoriously challenging in ice sheet modeling. Here we evaluate how an ice sheet system model responds to a given forcing. We show that hindcasting, i.e. forcing a model with known or closely estimated inputs for past events to see how wel...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: A. Aschwanden, G. A&#240algeirsdóttir, C. Khroulev
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-7-1083-2013
http://www.the-cryosphere.net/7/1083/2013/tc-7-1083-2013.pdf
https://doaj.org/article/0613998641b248db9a07ccecc3930ee9
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:0613998641b248db9a07ccecc3930ee9 2023-05-15T16:29:23+02:00 Hindcasting to measure ice sheet model sensitivity to initial states A. Aschwanden G. A&#240algeirsdóttir C. Khroulev 2013-07-01 https://doi.org/10.5194/tc-7-1083-2013 http://www.the-cryosphere.net/7/1083/2013/tc-7-1083-2013.pdf https://doaj.org/article/0613998641b248db9a07ccecc3930ee9 en eng Copernicus Publications doi:10.5194/tc-7-1083-2013 1994-0416 1994-0424 http://www.the-cryosphere.net/7/1083/2013/tc-7-1083-2013.pdf https://doaj.org/article/0613998641b248db9a07ccecc3930ee9 undefined The Cryosphere, Vol 7, Iss 4, Pp 1083-1093 (2013) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2013 fttriple https://doi.org/10.5194/tc-7-1083-2013 2023-01-22T19:31:04Z Validation is a critical component of model development, yet notoriously challenging in ice sheet modeling. Here we evaluate how an ice sheet system model responds to a given forcing. We show that hindcasting, i.e. forcing a model with known or closely estimated inputs for past events to see how well the output matches observations, is a viable method of assessing model performance. By simulating the recent past of Greenland, and comparing to observations of ice thickness, ice discharge, surface speeds, mass loss and surface elevation changes for validation, we find that the short term model response is strongly influenced by the initial state. We show that the thermal and dynamical states (i.e. the distribution of internal energy and momentum) can be misrepresented despite a good agreement with some observations, stressing the importance of using multiple observations. In particular we identify rates of change of spatially dense observations as preferred validation metrics. Hindcasting enables a qualitative assessment of model performance relative to observed rates of change. It thereby reduces the number of admissible initial states more rigorously than validation efforts that do not take advantage of observed rates of change. Article in Journal/Newspaper Greenland Ice Sheet The Cryosphere Unknown Greenland The Cryosphere 7 4 1083 1093
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
A. Aschwanden
G. A&#240algeirsdóttir
C. Khroulev
Hindcasting to measure ice sheet model sensitivity to initial states
topic_facet geo
envir
description Validation is a critical component of model development, yet notoriously challenging in ice sheet modeling. Here we evaluate how an ice sheet system model responds to a given forcing. We show that hindcasting, i.e. forcing a model with known or closely estimated inputs for past events to see how well the output matches observations, is a viable method of assessing model performance. By simulating the recent past of Greenland, and comparing to observations of ice thickness, ice discharge, surface speeds, mass loss and surface elevation changes for validation, we find that the short term model response is strongly influenced by the initial state. We show that the thermal and dynamical states (i.e. the distribution of internal energy and momentum) can be misrepresented despite a good agreement with some observations, stressing the importance of using multiple observations. In particular we identify rates of change of spatially dense observations as preferred validation metrics. Hindcasting enables a qualitative assessment of model performance relative to observed rates of change. It thereby reduces the number of admissible initial states more rigorously than validation efforts that do not take advantage of observed rates of change.
format Article in Journal/Newspaper
author A. Aschwanden
G. A&#240algeirsdóttir
C. Khroulev
author_facet A. Aschwanden
G. A&#240algeirsdóttir
C. Khroulev
author_sort A. Aschwanden
title Hindcasting to measure ice sheet model sensitivity to initial states
title_short Hindcasting to measure ice sheet model sensitivity to initial states
title_full Hindcasting to measure ice sheet model sensitivity to initial states
title_fullStr Hindcasting to measure ice sheet model sensitivity to initial states
title_full_unstemmed Hindcasting to measure ice sheet model sensitivity to initial states
title_sort hindcasting to measure ice sheet model sensitivity to initial states
publisher Copernicus Publications
publishDate 2013
url https://doi.org/10.5194/tc-7-1083-2013
http://www.the-cryosphere.net/7/1083/2013/tc-7-1083-2013.pdf
https://doaj.org/article/0613998641b248db9a07ccecc3930ee9
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
The Cryosphere
genre_facet Greenland
Ice Sheet
The Cryosphere
op_source The Cryosphere, Vol 7, Iss 4, Pp 1083-1093 (2013)
op_relation doi:10.5194/tc-7-1083-2013
1994-0416
1994-0424
http://www.the-cryosphere.net/7/1083/2013/tc-7-1083-2013.pdf
https://doaj.org/article/0613998641b248db9a07ccecc3930ee9
op_rights undefined
op_doi https://doi.org/10.5194/tc-7-1083-2013
container_title The Cryosphere
container_volume 7
container_issue 4
container_start_page 1083
op_container_end_page 1093
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