Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves
Calving mechanisms are still poorly understood and stress states in the vicinity of ice-shelf fronts are insufficiently known for the development of physically motivated calving laws that match observations. A calving model requires the knowledge of maximum tensile stresses. These stresses depend on...
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INT GLACIOL SOC
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ftawi:oai:epic.awi.de:40947 2023-05-15T13:29:47+02:00 Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves Christmann, Julia Plate, C. Müller, Ralf Humbert, Angelika 2016 application/pdf https://epic.awi.de/id/eprint/40947/ https://epic.awi.de/id/eprint/40947/1/viscous-and-viscoelastic-stress-states-at-the-calving-front-of-antarctic-ice-shelves.pdf https://hdl.handle.net/10013/epic.48952 https://hdl.handle.net/10013/epic.48952.d001 unknown INT GLACIOL SOC https://epic.awi.de/id/eprint/40947/1/viscous-and-viscoelastic-stress-states-at-the-calving-front-of-antarctic-ice-shelves.pdf https://hdl.handle.net/10013/epic.48952.d001 Christmann, J. , Plate, C. , Müller, R. and Humbert, A. (2016) Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves , Annals of Glaciology, 57 (73), pp. 10-18 . doi:10.1017/aog.2016.18 <https://doi.org/10.1017/aog.2016.18> , hdl:10013/epic.48952 EPIC3Annals of Glaciology, INT GLACIOL SOC, 57(73), pp. 10-18, ISSN: 0260-3055 Article isiRev 2016 ftawi https://doi.org/10.1017/aog.2016.18 2021-12-24T15:41:35Z Calving mechanisms are still poorly understood and stress states in the vicinity of ice-shelf fronts are insufficiently known for the development of physically motivated calving laws that match observations. A calving model requires the knowledge of maximum tensile stresses. These stresses depend on different simulation approaches and material models. Therefore, this study compares results of a two-dimensional (2-D) continuum approach using finite elements with results of a one- dimensional (1-D) beam model elaborated in Reeh (1968). A purely viscous model, as well as a viscoelas- tic Maxwell model, is applied for the 2-D case. The maximum tensile stress usually appears at the top surface of an ice shelf. Its location and magnitude are predominantly influenced by the thickness of the ice shelf and the height of the freeboard, the traction-free part at the ice front. More precisely, doub- ling the thickness leads to twice the stress maximum, while doubling the freeboard, based on changes of the ice density, results in an increase of the stress maximum by 61%. Poisson’s ratio controls the evolu- tion of the maximum stress with time. The viscosity and Young’s modulus define the characteristic time of the Maxwell model and thus the time to reach the maximum principal stress. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctic Ice Shelf Ice Shelves Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Antarctic Annals of Glaciology 57 73 10 18 |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
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Calving mechanisms are still poorly understood and stress states in the vicinity of ice-shelf fronts are insufficiently known for the development of physically motivated calving laws that match observations. A calving model requires the knowledge of maximum tensile stresses. These stresses depend on different simulation approaches and material models. Therefore, this study compares results of a two-dimensional (2-D) continuum approach using finite elements with results of a one- dimensional (1-D) beam model elaborated in Reeh (1968). A purely viscous model, as well as a viscoelas- tic Maxwell model, is applied for the 2-D case. The maximum tensile stress usually appears at the top surface of an ice shelf. Its location and magnitude are predominantly influenced by the thickness of the ice shelf and the height of the freeboard, the traction-free part at the ice front. More precisely, doub- ling the thickness leads to twice the stress maximum, while doubling the freeboard, based on changes of the ice density, results in an increase of the stress maximum by 61%. Poisson’s ratio controls the evolu- tion of the maximum stress with time. The viscosity and Young’s modulus define the characteristic time of the Maxwell model and thus the time to reach the maximum principal stress. |
format |
Article in Journal/Newspaper |
author |
Christmann, Julia Plate, C. Müller, Ralf Humbert, Angelika |
spellingShingle |
Christmann, Julia Plate, C. Müller, Ralf Humbert, Angelika Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves |
author_facet |
Christmann, Julia Plate, C. Müller, Ralf Humbert, Angelika |
author_sort |
Christmann, Julia |
title |
Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves |
title_short |
Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves |
title_full |
Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves |
title_fullStr |
Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves |
title_full_unstemmed |
Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves |
title_sort |
viscous and viscoelastic stress states at the calving front of antarctic ice shelves |
publisher |
INT GLACIOL SOC |
publishDate |
2016 |
url |
https://epic.awi.de/id/eprint/40947/ https://epic.awi.de/id/eprint/40947/1/viscous-and-viscoelastic-stress-states-at-the-calving-front-of-antarctic-ice-shelves.pdf https://hdl.handle.net/10013/epic.48952 https://hdl.handle.net/10013/epic.48952.d001 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Annals of Glaciology Antarc* Antarctic Ice Shelf Ice Shelves |
genre_facet |
Annals of Glaciology Antarc* Antarctic Ice Shelf Ice Shelves |
op_source |
EPIC3Annals of Glaciology, INT GLACIOL SOC, 57(73), pp. 10-18, ISSN: 0260-3055 |
op_relation |
https://epic.awi.de/id/eprint/40947/1/viscous-and-viscoelastic-stress-states-at-the-calving-front-of-antarctic-ice-shelves.pdf https://hdl.handle.net/10013/epic.48952.d001 Christmann, J. , Plate, C. , Müller, R. and Humbert, A. (2016) Viscous and viscoelastic stress states at the calving front of Antarctic ice shelves , Annals of Glaciology, 57 (73), pp. 10-18 . doi:10.1017/aog.2016.18 <https://doi.org/10.1017/aog.2016.18> , hdl:10013/epic.48952 |
op_doi |
https://doi.org/10.1017/aog.2016.18 |
container_title |
Annals of Glaciology |
container_volume |
57 |
container_issue |
73 |
container_start_page |
10 |
op_container_end_page |
18 |
_version_ |
1766003123060473856 |