Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Conrad P. Koziol"'
Publikováno v:
Koziol, C P, Todd, J A, Goldberg, D N & Maddison, J R 2021, ' fenics_ice 1.0: A framework for quantifying initialisation uncertainty for time-dependent ice-sheet models ', Geoscientific Model Development . https://doi.org/10.5194/gmd-14-5843-2021
Geoscientific Model Development, Vol 14, Pp 5843-5861 (2021)
Geoscientific Model Development, Vol 14, Pp 5843-5861 (2021)
Mass loss due to dynamic changes in ice sheets is a significant contributor to sea level rise, and this contribution is expectedto increase in the future. Numerical codes simulating the evolution of ice sheets can potentially quantify this future con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::18b73e1a94f8793164769458980fcd01
https://doi.org/10.5194/gmd-14-5843-2021
https://doi.org/10.5194/gmd-14-5843-2021
Mass loss due to dynamic changes in ice sheets is a significant contributor to sea level rise, and this contribution is expected to increase in the future. Numerical codes simulating the evolution of ice sheets can potentially quantify this future co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::493d9bf15b8da6449927126c336ea524
https://doi.org/10.5194/gmd-2021-90
https://doi.org/10.5194/gmd-2021-90
Autor:
Neil Arnold, Conrad P. Koziol
Publikováno v:
Koziol, C & Arnold, N 2018, ' Modelling seasonal meltwater forcing of the velocity of land-terminating margins of the Greenland Ice Sheet ', Cryosphere . https://doi.org/10.5194/tc-12-971-2018
The Cryosphere, Vol 12, Pp 971-991 (2018)
The Cryosphere, Vol 12, Pp 971-991 (2018)
Surface runoff at the margin of the Greenland Ice Sheet (GrIS) drains to the ice-sheet bed, leading to enhanced summer ice flow. Ice velocities show a pattern of early summer acceleration followed by mid-summer deceleration due to evolution of the su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::185c2a94953d4f497a90f25289474754
https://doi.org/10.5194/tc-12-971-2018
https://doi.org/10.5194/tc-12-971-2018
Autor:
Neil Arnold, Conrad P. Koziol
Publikováno v:
The Cryosphere, Vol 11, Pp 2783-2797 (2017)
Koziol, C & Arnold, N 2017, ' Incorporating modelled subglacial hydrology into inversions for basal drag ', Cryosphere Discussions . https://doi.org/10.5194/tc-11-2783-2017
Koziol, C & Arnold, N 2017, ' Incorporating modelled subglacial hydrology into inversions for basal drag ', Cryosphere Discussions . https://doi.org/10.5194/tc-11-2783-2017
A key challenge in modelling coupled ice flow – subglacial hydrology is initializing the state and parameters of the system. We address this problem by presenting a workflow for initializing these values at the start of a summer melt season. The wo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9719897e43856d054e3985d51f632600
https://www.the-cryosphere.net/11/2783/2017/tc-11-2783-2017.pdf
https://www.the-cryosphere.net/11/2783/2017/tc-11-2783-2017.pdf
Publikováno v:
Koziol, C, Arnold, N, Pope, A & Colgan, W 2017, ' Quantifying supraglacial meltwater pathways in the Paakitsoq region, West Greenland ', Journal of Glaciology . https://doi.org/10.1017/jog.2017.5
Increased summer ice velocities on the Greenland ice sheet are driven by meltwater input to the subglacial environment. However, spatial patterns of surface input and partitioning of meltwater between different pathways to the base remain poorly unde
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3520b1985feec59ec81d3afeb1942eb1