Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Alison J. Cook"'
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-11 (2024)
Abstract Arctic sea ice has shifted from a perennial (older, thicker ice) to a seasonal (younger, thinner) ice regime, leading to the increasingly common belief that shipping through Canada’s Northwest Passage is becoming more viable. Here, we use
Externí odkaz:
https://doaj.org/article/a78082bbfb6348b8ac2e05d4b217a4af
Autor:
David G. Vaughan, Paul R. Holland, Alison J. Cook, Michael P. Meredith, Adrian Luckman, Tavi Murray
Publikováno v:
Science, 2016, Vol.353(6296), pp.283-286 [Peer Reviewed Journal]
The heat is on Rising surface air temperatures are understood to cause glacial melting, but it is becoming increasingly clear that the ocean also has a strong impact. Cook et al. studied glaciers that drain the Antarctic Peninsula and found a strong
Autor:
Daniela Jansen, Alison J. Cook, Adrian Luckman, Bernd Kulessa, Bryn Hubbard, Suzanne Bevan, Paul R. Holland
Publikováno v:
The Cryosphere, Vol 9, Iss 3, Pp 1223-1227 (2015)
The Cryosphere, 2015, Vol.9(3), pp.1223-1227 [Peer Reviewed Journal]
EPIC3The Cryosphere, COPERNICUS GESELLSCHAFT MBH, 9, pp. 1223-1227, ISSN: 1994-0416
The Cryosphere, 2015, Vol.9(3), pp.1223-1227 [Peer Reviewed Journal]
EPIC3The Cryosphere, COPERNICUS GESELLSCHAFT MBH, 9, pp. 1223-1227, ISSN: 1994-0416
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://explore.openaire.eu/search/publication?articleId=doi_dedup___::4acb16809803deeff62ac75de3db1750
https://www.the-cryosphere.net/9/1223/2015/
https://www.the-cryosphere.net/9/1223/2015/
The glaciers on the Antarctic Peninsula (AP) potentially make a large contribution to sea level rise. However, this contribution has been difficult to estimate, as no complete glacier inventory (outlines, attributes, separation from the ice sheet) ha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::176af1105ef0cc56e0417c1507831358
https://doi.org/10.5167/uzh-127496
https://doi.org/10.5167/uzh-127496
Publikováno v:
Global Change Biology. 16:2614-2623
Feedbacks on climate change so far identified are predominantly positive, enhancing the rate of change. Loss of sea-ice, increase in desert areas, water vapour increase, loss of tropical rain forest and the restriction of significant areas of marine
Publikováno v:
Antarctic Science. 19:131-142
George VI Ice Shelf is the largest ice shelf on the west coast of the Antarctic Peninsula, covering a total area of 25 000 km2. The northern ice front of George VI Ice Shelf presently marks the southernmost occurrence of recent ice-shelf retreat on t
Publikováno v:
Science. 308:541-544
The continued retreat of ice shelves on the Antarctic Peninsula has been widely attributed to recent atmospheric warming, but there is little published work describing changes in glacier margin positions. We present trends in 244 marine glacier front
Autor:
R. Le Bris, Johannes Oerlemans, P. W. Leclercq, Alison J. Cook, Hassan J. Basagic, Irina Bushueva
Publikováno v:
The cryosphere, 2014, Vol.8(2), pp.659-672 [Peer Reviewed Journal]
The Cryosphere, Vol 8, Iss 2, Pp 659-672 (2014)
The Cryosphere, Vol 8, Iss 2, Pp 659-672 (2014)
Glacier fluctuations contribute to variations in sea level and historical glacier length fluctuations are natural indicators of past climate change. To study these subjects, long-term information of glacier change is needed. In this paper we present
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aaedf2397b54871ba139292142ee5b3b
https://doi.org/10.5194/tc-8-659-2014
https://doi.org/10.5194/tc-8-659-2014
Publikováno v:
Antarctic science, 2014, Vol.26(06), pp.614-624 [Peer Reviewed Journal]
Glaciers on the Antarctic Peninsula have recently shown changes in extent, velocity and thickness, yet there is little quantification of change in the mass balance of individual glaciers or the processes controlling changes in extent. Here a high-res
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c10cda335d590361ab36d794862fb350
https://cronfa.swan.ac.uk/Record/cronfa21909/Download/0021909-15062015085650.pdf
https://cronfa.swan.ac.uk/Record/cronfa21909/Download/0021909-15062015085650.pdf