A new vertically integrated MOno-Layer Higher-Order (MOLHO) ice flow model

Numerical simulations of ice sheets rely on the momentum balance to determine how ice velocities change as the geometry of the system evolves. Ice is generally assumed to follow a Stokes flow with a nonlinear viscosity. Several approximations have been proposed in order to lower the computational co...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: Dias dos Santos, Thiago, Morlighem, Mathieu, Brinkerhoff, Douglas
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-16-179-2022
https://noa.gwlb.de/receive/cop_mods_00059951
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00059600/tc-16-179-2022.pdf
https://tc.copernicus.org/articles/16/179/2022/tc-16-179-2022.pdf
id ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00059951
record_format openpolar
spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00059951 2024-09-15T18:39:00+00:00 A new vertically integrated MOno-Layer Higher-Order (MOLHO) ice flow model Dias dos Santos, Thiago Morlighem, Mathieu Brinkerhoff, Douglas 2022-01 electronic https://doi.org/10.5194/tc-16-179-2022 https://noa.gwlb.de/receive/cop_mods_00059951 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00059600/tc-16-179-2022.pdf https://tc.copernicus.org/articles/16/179/2022/tc-16-179-2022.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-16-179-2022 https://noa.gwlb.de/receive/cop_mods_00059951 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00059600/tc-16-179-2022.pdf https://tc.copernicus.org/articles/16/179/2022/tc-16-179-2022.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2022 ftnonlinearchiv https://doi.org/10.5194/tc-16-179-2022 2024-06-26T04:34:57Z Numerical simulations of ice sheets rely on the momentum balance to determine how ice velocities change as the geometry of the system evolves. Ice is generally assumed to follow a Stokes flow with a nonlinear viscosity. Several approximations have been proposed in order to lower the computational cost of a full-Stokes stress balance. A popular option is the Blatter–Pattyn or higher-order model (HO), which consists of a three-dimensional set of equations that solves the horizontal velocities only. However, it still remains computationally expensive for long transient simulations. Here we present a depth-integrated formulation of the HO model, which can be solved on a two-dimensional mesh in the horizontal plane. We employ a specific polynomial function to describe the vertical variation in the velocity, which allows us to integrate the vertical dimension using a semi-analytic integration. We assess the performance of this MOno-Layer Higher-Order (MOLHO) model to compute ice velocities and simulate grounding line dynamics on standard benchmarks (ISMIP-HOM and MISMIP3D). We compare MOLHO results to the ones obtained with the original three-dimensional HO model. We also compare the time performance of both models in time-dependent runs. Our results show that the ice velocities and grounding line positions obtained with MOLHO are in very good agreement with the ones from HO. In terms of computing time, MOLHO requires less than 10 % of the computational time of a typical HO model, for the same simulations. These results suggest that the MOno-Layer Higher-Order formulation provides improved computational time performance and a comparable accuracy compared to the HO formulation, which opens the door to higher-order paleo simulations. Article in Journal/Newspaper The Cryosphere Niedersächsisches Online-Archiv NOA The Cryosphere 16 1 179 195
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Dias dos Santos, Thiago
Morlighem, Mathieu
Brinkerhoff, Douglas
A new vertically integrated MOno-Layer Higher-Order (MOLHO) ice flow model
topic_facet article
Verlagsveröffentlichung
description Numerical simulations of ice sheets rely on the momentum balance to determine how ice velocities change as the geometry of the system evolves. Ice is generally assumed to follow a Stokes flow with a nonlinear viscosity. Several approximations have been proposed in order to lower the computational cost of a full-Stokes stress balance. A popular option is the Blatter–Pattyn or higher-order model (HO), which consists of a three-dimensional set of equations that solves the horizontal velocities only. However, it still remains computationally expensive for long transient simulations. Here we present a depth-integrated formulation of the HO model, which can be solved on a two-dimensional mesh in the horizontal plane. We employ a specific polynomial function to describe the vertical variation in the velocity, which allows us to integrate the vertical dimension using a semi-analytic integration. We assess the performance of this MOno-Layer Higher-Order (MOLHO) model to compute ice velocities and simulate grounding line dynamics on standard benchmarks (ISMIP-HOM and MISMIP3D). We compare MOLHO results to the ones obtained with the original three-dimensional HO model. We also compare the time performance of both models in time-dependent runs. Our results show that the ice velocities and grounding line positions obtained with MOLHO are in very good agreement with the ones from HO. In terms of computing time, MOLHO requires less than 10 % of the computational time of a typical HO model, for the same simulations. These results suggest that the MOno-Layer Higher-Order formulation provides improved computational time performance and a comparable accuracy compared to the HO formulation, which opens the door to higher-order paleo simulations.
format Article in Journal/Newspaper
author Dias dos Santos, Thiago
Morlighem, Mathieu
Brinkerhoff, Douglas
author_facet Dias dos Santos, Thiago
Morlighem, Mathieu
Brinkerhoff, Douglas
author_sort Dias dos Santos, Thiago
title A new vertically integrated MOno-Layer Higher-Order (MOLHO) ice flow model
title_short A new vertically integrated MOno-Layer Higher-Order (MOLHO) ice flow model
title_full A new vertically integrated MOno-Layer Higher-Order (MOLHO) ice flow model
title_fullStr A new vertically integrated MOno-Layer Higher-Order (MOLHO) ice flow model
title_full_unstemmed A new vertically integrated MOno-Layer Higher-Order (MOLHO) ice flow model
title_sort new vertically integrated mono-layer higher-order (molho) ice flow model
publisher Copernicus Publications
publishDate 2022
url https://doi.org/10.5194/tc-16-179-2022
https://noa.gwlb.de/receive/cop_mods_00059951
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00059600/tc-16-179-2022.pdf
https://tc.copernicus.org/articles/16/179/2022/tc-16-179-2022.pdf
genre The Cryosphere
genre_facet The Cryosphere
op_relation The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424
https://doi.org/10.5194/tc-16-179-2022
https://noa.gwlb.de/receive/cop_mods_00059951
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00059600/tc-16-179-2022.pdf
https://tc.copernicus.org/articles/16/179/2022/tc-16-179-2022.pdf
op_rights https://creativecommons.org/licenses/by/4.0/
uneingeschränkt
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-16-179-2022
container_title The Cryosphere
container_volume 16
container_issue 1
container_start_page 179
op_container_end_page 195
_version_ 1810483390753800192