Zobrazeno 1 - 10
of 45
pro vyhledávání: '"M, Haseloff"'
Publikováno v:
The Cryosphere, Vol 12, Pp 2545-2568 (2018)
The amount of ice discharged by an ice stream depends on its width, and the widths of unconfined ice streams such as the Siple Coast ice streams in West Antarctica have been observed to evolve on decadal to centennial timescales. Thermally driven
Externí odkaz:
https://doaj.org/article/22cacc8632b94545a2d588acd8ee2894
Publikováno v:
The Cryosphere, Vol 8, Iss 3, Pp 959-976 (2014)
The presence of strong diurnal cycling in basal water pressure records obtained during the melt season is well established for many glaciers. The behaviour of the drainage system outside the melt season is less well understood. Here we present boreho
Externí odkaz:
https://doaj.org/article/858b8c93176745758636220d4d23011c
Publikováno v:
The Cryosphere, Vol 6, Iss 2, Pp 273-286 (2012)
Recently observed large-scale disintegration of Antarctic ice shelves has moved their fronts closer towards grounded ice. In response, ice-sheet discharge into the ocean has accelerated, contributing to global sea-level rise and emphasizing the impor
Externí odkaz:
https://doaj.org/article/9d4846f3d25c4415adc3c77b9e58160c
Publikováno v:
The Cryosphere, Vol 5, Iss 3, Pp 727-740 (2011)
We present a dynamic equilibrium simulation of the ice sheet-shelf system on Antarctica with the Potsdam Parallel Ice Sheet Model (PISM-PIK). The simulation is initialized with present-day conditions for bed topography and ice thickness and then run
Externí odkaz:
https://doaj.org/article/c35a22712533459a8f69e53d9525a4e3
Publikováno v:
The Cryosphere, Vol 5, Iss 3, Pp 715-726 (2011)
We present the Potsdam Parallel Ice Sheet Model (PISM-PIK), developed at the Potsdam Institute for Climate Impact Research to be used for simulations of large-scale ice sheet-shelf systems. It is derived from the Parallel Ice Sheet Model (Bueler and
Externí odkaz:
https://doaj.org/article/c8078fa5e41045d09cb58eea2f81f0ea
Publikováno v:
The Cryosphere, Vol 5, Iss 1, Pp 35-44 (2011)
A parameterization for the motion of ice-shelf fronts on a Cartesian grid in finite-difference land-ice models is presented. The scheme prevents artificial thinning of the ice shelf at its edge, which occurs due to the finite resolution of the model.
Externí odkaz:
https://doaj.org/article/263116a6550d41b0a955eb4da0e7aee2
Autor:
N D, Modi, N O, Danell, R N A, Perry, A Y, Abuhelwa, A, Rathod, S, Badaoui, R A, McKinnon, M, Haseloff, A, Shahnam, S M, Swain, M, Welslau, M J, Sorich, A M, Hopkins
Publikováno v:
ESMO Open. 7:100475
The prognostic value of patient-reported outcomes (PROs) has been minimally explored in advanced breast cancer (BC), and their comparative prognostic performance against Eastern Cooperative Oncology Group performance status (ECOG PS) is largely unkno
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