Zobrazeno 1 - 10
of 76
pro vyhledávání: '"C R Stokes"'
Publikováno v:
The Cryosphere, Vol 17, Pp 3593-3616 (2023)
Wilkes Land, East Antarctica, has been losing mass at an accelerating rate over recent decades in response to enhanced oceanic forcing. Overlying the Aurora Subglacial Basin, it has been referred to as the “weak underbelly” of the East Antarctic
Externí odkaz:
https://doaj.org/article/c9ab9a6fd06a4fa887fd38fb61edd5d3
Autor:
James R. Jordan, B. W. J. Miles, G. H. Gudmundsson, S. S. R. Jamieson, A. Jenkins, C. R. Stokes
Publikováno v:
Nature Communications, Vol 14, Iss 1, Pp 1-11 (2023)
The East Antarctic Ice Sheet is currently surrounded by relatively cool water but changes in ocean dynamics may lead to warmer ocean water on the shelf in the future. This has the potential to dramatically increase its future sea level contribution.
Externí odkaz:
https://doaj.org/article/7fb4a2a2d972401698a3ab2887a2c096
Publikováno v:
The Cryosphere, Vol 17, Pp 445-456 (2023)
Around large parts of West Antarctica and in Wilkes Land, East Antarctica, increased wind-forced intrusions of modified Circumpolar Deep Water (mCDW) onto the continental shelf have been associated with mass loss over the last few decades. Despite co
Externí odkaz:
https://doaj.org/article/ce80afe5b34549b598ca3ee611dd2702
Publikováno v:
Journal of Maps, Vol 17, Iss 2, Pp 348-366 (2021)
Here we present a glacial and periglacial geomorphological map of a ∼6800 km2 region of central Troms and Finnmark county, Arctic Norway. The map is presented at a 1:115,000 scale with the aim of characterising the spatial distribution of glacial a
Externí odkaz:
https://doaj.org/article/e8871bf08cbc4f62912c0cd1d6ccbc63
Publikováno v:
The Cryosphere, Vol 15, Pp 5041-5059 (2021)
A wealth of research has focused on elucidating the key controls on mass loss from the Greenland and Antarctic ice sheets in response to climate forcing, specifically in relation to the drivers of marine-terminating outlet glacier change. The manual
Externí odkaz:
https://doaj.org/article/55e9c0b8bc2a4ccbab427d49f4413526
Publikováno v:
The Cryosphere, Vol 15, Pp 663-676 (2021)
After Totten, Denman Glacier is the largest contributor to sea level rise in East Antarctica. Denman's catchment contains an ice volume equivalent to 1.5 m of global sea level and sits in the Aurora Subglacial Basin (ASB). Geological evidence of this
Externí odkaz:
https://doaj.org/article/35c3f50e118b4e299c3c4f9d2e98cc01
Publikováno v:
The Cryosphere, Vol 14, Pp 4103-4120 (2020)
Supraglacial lakes (SGLs) enhance surface melting and can flex and fracture ice shelves when they grow and subsequently drain, potentially leading to ice shelf disintegration. However, the seasonal evolution of SGLs and their influence on ice shelf s
Externí odkaz:
https://doaj.org/article/d34b377caa59459c9dbbe1f53dcfedbb
Publikováno v:
Journal of Glaciology, Vol 66, Pp 485-495 (2020)
Evolving conditions at the terminus of Thwaites Glacier will be important in determining the rate of its future sea-level contribution over the coming decades. Here, we use remote-sensing observations to investigate recent changes (2000–2018) in th
Externí odkaz:
https://doaj.org/article/677174237ff14db2b755dcb18c648538
Publikováno v:
Arctic, Antarctic, and Alpine Research, Vol 52, Iss 1, Pp 281-311 (2020)
Glaciers are important indicators of climate change, and recent observations worldwide document increasing rates of mountain glacier recession. Here we present approximately 200 years of change in mountain glacier extent in northern Troms and western
Externí odkaz:
https://doaj.org/article/b440cf6d994e4b3fafa96df6a2457682
Publikováno v:
Journal of Glaciology, Vol 65, Pp 873-888 (2019)
Small mountain glaciers are an important part of the cryosphere and tend to respond rapidly to climate warming. Historically, mapping very small glaciers (generally considered to be
Externí odkaz:
https://doaj.org/article/fd5c494342e54d68a501ee8545c72c69