Multiscale modeling of ice deformation behavior
Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Montagnat, M. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014transfer abstract |
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| Schlagwörter: |
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| Umfang: |
31 |
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| Übergeordnetes Werk: |
Enthalten in: Pneumococcal Vaccination Coverage Among Adults with Work-Related Asthma, Asthma Call-Back Survey, 29 States, 2012–2013 - Dodd, Katelynn ELSEVIER, 2017, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:61 ; year:2014 ; pages:78-108 ; extent:31 |
| Links: |
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| DOI / URN: |
10.1016/j.jsg.2013.05.002 |
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ELV039252159 |
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| 520 | |a Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. | ||
| 520 | |a Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. | ||
| 650 | 7 | |a Ice mechanical behavior |2 Elsevier | |
| 650 | 7 | |a Viscoplastic anisotropy |2 Elsevier | |
| 650 | 7 | |a Multiscale modeling |2 Elsevier | |
| 650 | 7 | |a Fabric development |2 Elsevier | |
| 700 | 1 | |a Castelnau, O. |4 oth | |
| 700 | 1 | |a Bons, P.D. |4 oth | |
| 700 | 1 | |a Faria, S.H. |4 oth | |
| 700 | 1 | |a Gagliardini, O. |4 oth | |
| 700 | 1 | |a Gillet-Chaulet, F. |4 oth | |
| 700 | 1 | |a Grennerat, F. |4 oth | |
| 700 | 1 | |a Griera, A. |4 oth | |
| 700 | 1 | |a Lebensohn, R.A. |4 oth | |
| 700 | 1 | |a Moulinec, H. |4 oth | |
| 700 | 1 | |a Roessiger, J. |4 oth | |
| 700 | 1 | |a Suquet, P. |4 oth | |
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10.1016/j.jsg.2013.05.002 doi GBVA2014006000020.pica (DE-627)ELV039252159 (ELSEVIER)S0191-8141(13)00083-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 610 VZ 44.85 bkl Montagnat, M. verfasserin aut Multiscale modeling of ice deformation behavior 2014transfer abstract 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Ice mechanical behavior Elsevier Viscoplastic anisotropy Elsevier Multiscale modeling Elsevier Fabric development Elsevier Castelnau, O. oth Bons, P.D. oth Faria, S.H. oth Gagliardini, O. oth Gillet-Chaulet, F. oth Grennerat, F. oth Griera, A. oth Lebensohn, R.A. oth Moulinec, H. oth Roessiger, J. oth Suquet, P. oth Enthalten in Elsevier Science Dodd, Katelynn ELSEVIER Pneumococcal Vaccination Coverage Among Adults with Work-Related Asthma, Asthma Call-Back Survey, 29 States, 2012–2013 2017 Amsterdam [u.a.] (DE-627)ELV014727196 volume:61 year:2014 pages:78-108 extent:31 https://doi.org/10.1016/j.jsg.2013.05.002 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 44.85 Kardiologie Angiologie VZ AR 61 2014 78-108 31 045F 550 |
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10.1016/j.jsg.2013.05.002 doi GBVA2014006000020.pica (DE-627)ELV039252159 (ELSEVIER)S0191-8141(13)00083-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 610 VZ 44.85 bkl Montagnat, M. verfasserin aut Multiscale modeling of ice deformation behavior 2014transfer abstract 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Ice mechanical behavior Elsevier Viscoplastic anisotropy Elsevier Multiscale modeling Elsevier Fabric development Elsevier Castelnau, O. oth Bons, P.D. oth Faria, S.H. oth Gagliardini, O. oth Gillet-Chaulet, F. oth Grennerat, F. oth Griera, A. oth Lebensohn, R.A. oth Moulinec, H. oth Roessiger, J. oth Suquet, P. oth Enthalten in Elsevier Science Dodd, Katelynn ELSEVIER Pneumococcal Vaccination Coverage Among Adults with Work-Related Asthma, Asthma Call-Back Survey, 29 States, 2012–2013 2017 Amsterdam [u.a.] (DE-627)ELV014727196 volume:61 year:2014 pages:78-108 extent:31 https://doi.org/10.1016/j.jsg.2013.05.002 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 44.85 Kardiologie Angiologie VZ AR 61 2014 78-108 31 045F 550 |
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10.1016/j.jsg.2013.05.002 doi GBVA2014006000020.pica (DE-627)ELV039252159 (ELSEVIER)S0191-8141(13)00083-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 610 VZ 44.85 bkl Montagnat, M. verfasserin aut Multiscale modeling of ice deformation behavior 2014transfer abstract 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Ice mechanical behavior Elsevier Viscoplastic anisotropy Elsevier Multiscale modeling Elsevier Fabric development Elsevier Castelnau, O. oth Bons, P.D. oth Faria, S.H. oth Gagliardini, O. oth Gillet-Chaulet, F. oth Grennerat, F. oth Griera, A. oth Lebensohn, R.A. oth Moulinec, H. oth Roessiger, J. oth Suquet, P. oth Enthalten in Elsevier Science Dodd, Katelynn ELSEVIER Pneumococcal Vaccination Coverage Among Adults with Work-Related Asthma, Asthma Call-Back Survey, 29 States, 2012–2013 2017 Amsterdam [u.a.] (DE-627)ELV014727196 volume:61 year:2014 pages:78-108 extent:31 https://doi.org/10.1016/j.jsg.2013.05.002 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 44.85 Kardiologie Angiologie VZ AR 61 2014 78-108 31 045F 550 |
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10.1016/j.jsg.2013.05.002 doi GBVA2014006000020.pica (DE-627)ELV039252159 (ELSEVIER)S0191-8141(13)00083-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 610 VZ 44.85 bkl Montagnat, M. verfasserin aut Multiscale modeling of ice deformation behavior 2014transfer abstract 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Ice mechanical behavior Elsevier Viscoplastic anisotropy Elsevier Multiscale modeling Elsevier Fabric development Elsevier Castelnau, O. oth Bons, P.D. oth Faria, S.H. oth Gagliardini, O. oth Gillet-Chaulet, F. oth Grennerat, F. oth Griera, A. oth Lebensohn, R.A. oth Moulinec, H. oth Roessiger, J. oth Suquet, P. oth Enthalten in Elsevier Science Dodd, Katelynn ELSEVIER Pneumococcal Vaccination Coverage Among Adults with Work-Related Asthma, Asthma Call-Back Survey, 29 States, 2012–2013 2017 Amsterdam [u.a.] (DE-627)ELV014727196 volume:61 year:2014 pages:78-108 extent:31 https://doi.org/10.1016/j.jsg.2013.05.002 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 44.85 Kardiologie Angiologie VZ AR 61 2014 78-108 31 045F 550 |
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10.1016/j.jsg.2013.05.002 doi GBVA2014006000020.pica (DE-627)ELV039252159 (ELSEVIER)S0191-8141(13)00083-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 610 VZ 44.85 bkl Montagnat, M. verfasserin aut Multiscale modeling of ice deformation behavior 2014transfer abstract 31 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. Ice mechanical behavior Elsevier Viscoplastic anisotropy Elsevier Multiscale modeling Elsevier Fabric development Elsevier Castelnau, O. oth Bons, P.D. oth Faria, S.H. oth Gagliardini, O. oth Gillet-Chaulet, F. oth Grennerat, F. oth Griera, A. oth Lebensohn, R.A. oth Moulinec, H. oth Roessiger, J. oth Suquet, P. oth Enthalten in Elsevier Science Dodd, Katelynn ELSEVIER Pneumococcal Vaccination Coverage Among Adults with Work-Related Asthma, Asthma Call-Back Survey, 29 States, 2012–2013 2017 Amsterdam [u.a.] (DE-627)ELV014727196 volume:61 year:2014 pages:78-108 extent:31 https://doi.org/10.1016/j.jsg.2013.05.002 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 44.85 Kardiologie Angiologie VZ AR 61 2014 78-108 31 045F 550 |
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Enthalten in Pneumococcal Vaccination Coverage Among Adults with Work-Related Asthma, Asthma Call-Back Survey, 29 States, 2012–2013 Amsterdam [u.a.] volume:61 year:2014 pages:78-108 extent:31 |
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Enthalten in Pneumococcal Vaccination Coverage Among Adults with Work-Related Asthma, Asthma Call-Back Survey, 29 States, 2012–2013 Amsterdam [u.a.] volume:61 year:2014 pages:78-108 extent:31 |
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Pneumococcal Vaccination Coverage Among Adults with Work-Related Asthma, Asthma Call-Back Survey, 29 States, 2012–2013 |
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Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. |
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Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. |
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Understanding the flow of ice in glaciers and polar ice sheets is of increasing relevance in a time of potentially significant climate change. The flow of ice has hitherto received relatively little attention from the structural geological community. This paper aims to provide an overview of methods and results of ice deformation modeling from the single crystal to the polycrystal scale, and beyond to the scale of polar ice sheets. All through these scales, various models have been developed to understand, describe and predict the processes that operate during deformation of ice, with the aim to correctly represent ice rheology and self-induced anisotropy. Most of the modeling tools presented in this paper originate from the material science community, and are currently used and further developed for other materials and environments. We will show that this community has deeply integrated ice as a very useful “model” material to develop and validate approaches in conditions of a highly anisotropic behavior. This review, by no means exhaustive, aims at providing an overview of methods at different scales and levels of complexity. |
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