Zobrazeno 1 - 10
of 12
pro vyhledávání: '"C. P. BORSTAD"'
Autor:
D. M. McCLUNG, C. P. BORSTAD
Publikováno v:
Journal of Glaciology, Vol 65, Pp 157-167 (2019)
From field observations, dry snow slab avalanche initiation is associated with fracture within relatively thin weak layers under stronger, cohesive slabs. For risk-based avalanche prediction, it is important to understand the fracture properties of a
Externí odkaz:
https://doaj.org/article/e91feacb384a48a6a10b8bf6102d4f98
Publikováno v:
Geoscientific Model Development, Vol 10, Iss 1, Pp 155-168 (2017)
Identifying fast and robust numerical solvers is a critical issue that needs to be addressed in order to improve projections of polar ice sheets evolving in a changing climate. This work evaluates the impact of using advanced numerical solvers for tr
Externí odkaz:
https://doaj.org/article/7c8fa41810f74cfbabd260ae9fc224f6
Publikováno v:
The Cryosphere, Vol 7, Iss 6, Pp 1931-1947 (2013)
Around the perimeter of Antarctica, much of the ice sheet discharges to the ocean through floating ice shelves. The buttressing provided by ice shelves is critical for modulating the flux of ice into the ocean, and the presently observed thinning o
Externí odkaz:
https://doaj.org/article/d7f9ce2590bb4f81863e552dfae31e08
Autor:
C. P. Borstad, David M. McClung
Publikováno v:
Journal of Glaciology. 65:157-167
From field observations, dry snow slab avalanche initiation is associated with fracture within relatively thin weak layers under stronger, cohesive slabs. For risk-based avalanche prediction, it is important to understand the fracture properties of a
Publikováno v:
Habbal, F; Larour, E; Morlighem, M; Seroussi, H; Borstad, CP; & Rignot, E. (2017). Optimal numerical solvers for transient simulations of ice flow using the Ice Sheet System Model (ISSM versions 4.2.5 and 4.11). GEOSCIENTIFIC MODEL DEVELOPMENT, 10(1), 155-168. doi: 10.5194/gmd-10-155-2017. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/87x36380
Geoscientific Model Development, vol 10, iss 1
Geoscientific Model Development, Vol 10, Iss 1, Pp 155-168 (2017)
Geoscientific Model Development, vol 10, iss 1
Geoscientific Model Development, Vol 10, Iss 1, Pp 155-168 (2017)
Identifying fast and robust numerical solvers is a critical issue that needs to be addressed in order to improve projections of polar ice sheets evolving in a changing climate. This work evaluates the impact of using advanced numerical solvers for tr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::891a81ac74528a3c336377549017082e
https://www.geosci-model-dev.net/10/155/2017/
https://www.geosci-model-dev.net/10/155/2017/
Publikováno v:
Earth and Planetary Science Letters. 419:199-210
Following the 2002 disintegration of the northern and central parts of the Larsen B Ice Shelf, the tributary glaciers of the southern surviving part initially appeared relatively unchanged and hence assumed to be buttressed sufficiently by the remnan
Publikováno v:
Journal of Geophysical Research: Earth Surface. 119:1918-1935
Ice shelves play a major role in buttressing ice sheet flow into the ocean, hence the importance of accurate numerical modeling of their stress regime. Commonly used ice flow models assume a continuous medium and are therefore complicated by the pres
Autor:
C. P. Borstad, David M. McClung
Publikováno v:
Journal of Geophysical Research: Earth Surface. 118:900-912
[1] The tensile fracture of heterogeneous earth materials such as snow, ice, and rocks can be characterized by two fracture parameters—the fracture toughness and the fracture process zone length. The latter length scale characterizes the zone of mi
Identifying fast and robust numerical solvers is a critical issue that needs to be addressed in order to improve projections of polar ice sheets evolving in a changing climate. This work evaluates the impact of using sophisticated numerical solvers f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::73a1c68e98e3140d823e57ae2a7bf83d
https://doi.org/10.5194/gmd-2016-111
https://doi.org/10.5194/gmd-2016-111
Autor:
Ala Khazendar, Helene Seroussi, Eric Rignot, Eric Larour, C. P. Borstad, Mathieu Morlighem, M. Schodlok
Publikováno v:
Geophysical Research Letters. 39
Calving is a primary process of mass ablation for glaciers and ice sheets, though it still eludes a general physical law. Here, we propose a calving framework based on continuum damage mechanics coupled with the equations of viscous deformation of gl