Parameter and state estimation with a time-dependent adjoint marine ice sheet model

To date, assimilation of observations into large-scale ice models has consisted predominantly of time-independent inversions of surface velocities for basal traction, bed elevation, or ice stiffness, and has relied primarily on analytically derived adjoints of glaciological stress balance models. To...

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Published in:The Cryosphere
Main Authors: D. N. Goldberg, P. Heimbach
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:https://doi.org/10.5194/tc-7-1659-2013
https://doaj.org/article/bddcb24761e94074a5b03aae1380441c
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spelling ftdoajarticles:oai:doaj.org/article:bddcb24761e94074a5b03aae1380441c 2023-05-15T16:40:22+02:00 Parameter and state estimation with a time-dependent adjoint marine ice sheet model D. N. Goldberg P. Heimbach 2013-11-01T00:00:00Z https://doi.org/10.5194/tc-7-1659-2013 https://doaj.org/article/bddcb24761e94074a5b03aae1380441c EN eng Copernicus Publications http://www.the-cryosphere.net/7/1659/2013/tc-7-1659-2013.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 1994-0416 1994-0424 doi:10.5194/tc-7-1659-2013 https://doaj.org/article/bddcb24761e94074a5b03aae1380441c The Cryosphere, Vol 7, Iss 6, Pp 1659-1678 (2013) Environmental sciences GE1-350 Geology QE1-996.5 article 2013 ftdoajarticles https://doi.org/10.5194/tc-7-1659-2013 2022-12-31T02:14:53Z To date, assimilation of observations into large-scale ice models has consisted predominantly of time-independent inversions of surface velocities for basal traction, bed elevation, or ice stiffness, and has relied primarily on analytically derived adjoints of glaciological stress balance models. To overcome limitations of such "snapshot" inversions – i.e., their inability to assimilate time-dependent data for the purpose of constraining transient flow states, or to produce initial states with minimum artificial drift and suitable for time-dependent simulations – we have developed an adjoint of a time-dependent parallel glaciological flow model. The model implements a hybrid shallow shelf–shallow ice stress balance, solves the continuity equation for ice thickness evolution, and can represent the floating, fast-sliding, and frozen bed regimes of a marine ice sheet. The adjoint is generated by a combination of analytic methods and the use of algorithmic differentiation (AD) software. Several experiments are carried out with idealized geometries and synthetic observations, including inversion of time-dependent surface elevations for past thicknesses, and simultaneous retrieval of basal traction and topography from surface data. Flexible generation of the adjoint for a range of independent uncertain variables is exemplified through sensitivity calculations of grounded ice volume to changes in basal melting of floating and basal sliding of grounded ice. The results are encouraging and suggest the feasibility, using real observations, of improved ice sheet state estimation and comprehensive transient sensitivity assessments. Article in Journal/Newspaper Ice Sheet The Cryosphere Directory of Open Access Journals: DOAJ Articles The Cryosphere 7 6 1659 1678
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
D. N. Goldberg
P. Heimbach
Parameter and state estimation with a time-dependent adjoint marine ice sheet model
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description To date, assimilation of observations into large-scale ice models has consisted predominantly of time-independent inversions of surface velocities for basal traction, bed elevation, or ice stiffness, and has relied primarily on analytically derived adjoints of glaciological stress balance models. To overcome limitations of such "snapshot" inversions – i.e., their inability to assimilate time-dependent data for the purpose of constraining transient flow states, or to produce initial states with minimum artificial drift and suitable for time-dependent simulations – we have developed an adjoint of a time-dependent parallel glaciological flow model. The model implements a hybrid shallow shelf–shallow ice stress balance, solves the continuity equation for ice thickness evolution, and can represent the floating, fast-sliding, and frozen bed regimes of a marine ice sheet. The adjoint is generated by a combination of analytic methods and the use of algorithmic differentiation (AD) software. Several experiments are carried out with idealized geometries and synthetic observations, including inversion of time-dependent surface elevations for past thicknesses, and simultaneous retrieval of basal traction and topography from surface data. Flexible generation of the adjoint for a range of independent uncertain variables is exemplified through sensitivity calculations of grounded ice volume to changes in basal melting of floating and basal sliding of grounded ice. The results are encouraging and suggest the feasibility, using real observations, of improved ice sheet state estimation and comprehensive transient sensitivity assessments.
format Article in Journal/Newspaper
author D. N. Goldberg
P. Heimbach
author_facet D. N. Goldberg
P. Heimbach
author_sort D. N. Goldberg
title Parameter and state estimation with a time-dependent adjoint marine ice sheet model
title_short Parameter and state estimation with a time-dependent adjoint marine ice sheet model
title_full Parameter and state estimation with a time-dependent adjoint marine ice sheet model
title_fullStr Parameter and state estimation with a time-dependent adjoint marine ice sheet model
title_full_unstemmed Parameter and state estimation with a time-dependent adjoint marine ice sheet model
title_sort parameter and state estimation with a time-dependent adjoint marine ice sheet model
publisher Copernicus Publications
publishDate 2013
url https://doi.org/10.5194/tc-7-1659-2013
https://doaj.org/article/bddcb24761e94074a5b03aae1380441c
genre Ice Sheet
The Cryosphere
genre_facet Ice Sheet
The Cryosphere
op_source The Cryosphere, Vol 7, Iss 6, Pp 1659-1678 (2013)
op_relation http://www.the-cryosphere.net/7/1659/2013/tc-7-1659-2013.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
1994-0416
1994-0424
doi:10.5194/tc-7-1659-2013
https://doaj.org/article/bddcb24761e94074a5b03aae1380441c
op_doi https://doi.org/10.5194/tc-7-1659-2013
container_title The Cryosphere
container_volume 7
container_issue 6
container_start_page 1659
op_container_end_page 1678
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