Zobrazeno 1 - 10
of 185
pro vyhledávání: '"P. R. Holland"'
Publikováno v:
The Cryosphere, Vol 18, Pp 2653-2675 (2024)
The Amundsen Sea sector has some of the fastest-thinning ice shelves in Antarctica, caused by high, ocean-driven basal melt rates, which can lead to increased ice streamflow, causing increased sea level rise (SLR) contributions. In this study, we pre
Externí odkaz:
https://doaj.org/article/db97872ee69d478a851896721d51a542
Publikováno v:
The Cryosphere, Vol 17, Pp 4399-4420 (2023)
Glaciers in the Amundsen Sea Embayment of West Antarctica are rapidly retreating and contributing to sea level rise. Ice loss is occurring primarily via exposure to warm ocean water, which varies in response to local wind variability. There is eviden
Externí odkaz:
https://doaj.org/article/8352b2080d414b8ebef619e854170fd0
Publikováno v:
The Cryosphere, Vol 17, Pp 3203-3228 (2023)
A major source of uncertainty in future sea level projections is the ocean-driven basal melt of Antarctic ice shelves. While ice sheet models require a kilometre-scale resolution to realistically resolve ice shelf stability and grounding line migrati
Externí odkaz:
https://doaj.org/article/a80bdea00063411f97c8a0b8bb8717e5
Autor:
P. R. Holland, G. K. O'Connor, T. J. Bracegirdle, P. Dutrieux, K. A. Naughten, E. J. Steig, D. P. Schneider, A. Jenkins, J. A. Smith
Publikováno v:
The Cryosphere, Vol 16, Pp 5085-5105 (2022)
Ocean-driven ice loss from the West Antarctic Ice Sheet is a significant contributor to sea-level rise. Recent ocean variability in the Amundsen Sea is controlled by near-surface winds. We combine palaeoclimate reconstructions and climate model simul
Externí odkaz:
https://doaj.org/article/87bd7d19a48b4dc9ad9e1cd7c570135d
Autor:
A. Siahaan, R. S. Smith, P. R. Holland, A. Jenkins, J. M. Gregory, V. Lee, P. Mathiot, A. J. . Payne, J. K. . Ridley, C. G. Jones
Publikováno v:
The Cryosphere, Vol 16, Pp 4053-4086 (2022)
The Antarctic Ice Sheet will play a crucial role in the evolution of global mean sea level as the climate warms. An interactively coupled climate and ice sheet model is needed to understand the impacts of ice–climate feedbacks during this evolution
Externí odkaz:
https://doaj.org/article/df360f90269148b181055b409cd38204
Publikováno v:
The Cryosphere, Vol 13, Pp 265-280 (2019)
Persistent outflow of supercooled ice-shelf water (ISW) from beneath McMurdo Ice Shelf creates a rapidly growing sub-ice platelet layer (SIPL) with a unique crystallographic structure under the sea ice in McMurdo Sound, Antarctica. A vertically modif
Externí odkaz:
https://doaj.org/article/d112e1dc743c4007a21a25e0791ebea2
Autor:
A. A. Petty, J. C. Stroeve, P. R. Holland, L. N. Boisvert, A. C. Bliss, N. Kimura, W. N. Meier
Publikováno v:
The Cryosphere, Vol 12, Pp 433-452 (2018)
The Arctic sea ice cover of 2016 was highly noteworthy, as it featured record low monthly sea ice extents at the start of the year but a summer (September) extent that was higher than expected by most seasonal forecasts. Here we explore the 2016 A
Externí odkaz:
https://doaj.org/article/6557d65942fe4720ad529626eccba856
Autor:
X. S. Asay-Davis, S. L. Cornford, G. Durand, B. K. Galton-Fenzi, R. M. Gladstone, G. H. Gudmundsson, T. Hattermann, D. M. Holland, D. Holland, P. R. Holland, D. F. Martin, P. Mathiot, F. Pattyn, H. Seroussi
Publikováno v:
Geoscientific Model Development, Vol 9, Iss 7, Pp 2471-2497 (2016)
Coupled ice sheet–ocean models capable of simulating moving grounding lines are just becoming available. Such models have a broad range of potential applications in studying the dynamics of marine ice sheets and tidewater glaciers, from process stu
Externí odkaz:
https://doaj.org/article/49e54c33cdf7461bb818a35cac232c2e
Publikováno v:
The Cryosphere, Vol 9, Iss 3, Pp 1223-1227 (2015)
An established rift in the Larsen C Ice Shelf, formerly constrained by a suture zone containing marine ice, grew rapidly during 2014 and is likely in the near future to generate the largest calving event since the 1980s and result in a new minimum ar
Externí odkaz:
https://doaj.org/article/9d3e7407169040599b897437797c4578
Autor:
P. R. Holland, A. Brisbourne, H. F. J. Corr, D. McGrath, K. Purdon, J. Paden, H. A. Fricker, F. S. Paolo, A. H. Fleming
Publikováno v:
The Cryosphere, Vol 9, Iss 3, Pp 1005-1024 (2015)
The catastrophic collapses of Larsen A and B ice shelves on the eastern Antarctic Peninsula have caused their tributary glaciers to accelerate, contributing to sea-level rise and freshening the Antarctic Bottom Water formed nearby. The surface of Lar
Externí odkaz:
https://doaj.org/article/5d5ac2d9bfb043c29d1b1c0ede63b48c