Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Trudy Wohlleben"'
Autor:
Will Kochtitzky, Luke Copland, Trudy Wohlleben, Pilipoosie Iqaluk, Catherine Girard, Warwick F. Vincent, Alexander I. Culley
Publikováno v:
Arctic Science, Vol 9, Iss 2, Pp 451-464 (2023)
Relatively little is known about the glaciers of northern Ellesmere Island, Canada. Here we describe the first field and remote sensing observations of Thores Glacier, located 50 km inland from the Arctic Ocean. The glacier is slow-moving, with maxim
Externí odkaz:
https://doaj.org/article/d58390c45c2c4328a0b9f7644062a303
Autor:
Will Kochtitzky, Luke Copland, Trudy Wohlleben, Pilipoosie Iqaluk, Catherine Girard, Warwick F. Vincent, Alexander I. Culley
Publikováno v:
Arctic Science.
Relatively little is known about the glaciers of northern Ellesmere Island, Canada. Here we describe the first field and remote sensing observations of Thores Glacier, located 50 km inland from the Arctic Ocean. The glacier is slow-moving, with maxim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::304fcbf4c87482324ff44a09b06e0a8e
https://doi.org/10.1139/as-2022-0012
https://doi.org/10.1139/as-2022-0012
Autor:
Jia Wang, David J. Schwab, Xuezhi Bai, Lin Luo, Raymond Assel, Brent M. Lofgren, John F. Bratton, Jay A. Austin, Trudy Wohlleben, John D. Lenters, Anne H. Clites, Sean R. Helfrich, George Leshkevich, Henry A. Vanderploeg, Marie Colton
Publikováno v:
Climate Dynamics. 44:1187-1213
A record-breaking low ice cover occurred in the North American Great Lakes during winter 2011/2012, in conjunction with a strong positive Arctic Oscillation/North Atlantic Oscillation (+AO/NAO) and a La Nina event. Large-scale atmosphere circulation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55e5641707a47bcf7e308ade743aeb1f
https://doi.org/10.1007/s00382-014-2225-2
https://doi.org/10.1007/s00382-014-2225-2
Autor:
Stephen E. L. Howell, Chris Derksen, Trudy Wohlleben, Larissa Pizzolato, Mohammed Dabboor, Alexander Komarov
Publikováno v:
Journal of Geophysical Research: Oceans. 118:3595-3607
[1] Sea ice is exchanged between the Arctic Ocean and Canadian Arctic Archipelago (CAA) but has not been quantified over long time periods. The corresponding mechanisms responsible for recent variability and change also remain unidentified. To addres
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6fb7ba461b6ba3e228fa04313adcb09b
https://doi.org/10.1002/jgrc.20265
https://doi.org/10.1002/jgrc.20265
Autor:
Humfrey Melling, Eric Rignot, Jason E. Box, P. Gudmandsen, Trudy Wohlleben, Luke Copland, A.K. Higgins, Kelly K. Falkner, Andreas M. Münchow, Helen L. Johnson, Roger M. Samelson, Konrad Steffen
Publikováno v:
Falkner, KK; Melling, H; Mnchow, AM; Box, JE; Wohlleben, T; Johnson, HL; et al.(2011). Context for the recent massive petermann glacier calving event. Eos, 92(14), 117-118. doi: 10.1029/2011EO140001. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/0dt928rh
On 4 August 2010, about one fifth of the floating ice tongue of Petermann Glacier (also known as "Petermann Gletscher") in northwestern Greenland calved (Figure 1). The resulting "ice island" had an area approximately 4 times that of Manhattan Island
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3513b0e336af3aa17efb16c94936fd30
https://ora.ox.ac.uk/objects/uuid:b68af269-98cf-4076-bdad-199482ddd504
https://ora.ox.ac.uk/objects/uuid:b68af269-98cf-4076-bdad-199482ddd504
Publikováno v:
Atmosphere-Ocean. 51:1-17
One of the routes for thick, multi-year sea ice (MYI) exiting the Arctic Ocean is through the Queen Elizabeth Islands (QEI) in the Canadian Arctic. Quantifying the volume of MYI that passes through the QEI and the associated transit times is importan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bffd74db9a02e2fdb50ee6b856e78919
https://doi.org/10.1080/07055900.2012.750232
https://doi.org/10.1080/07055900.2012.750232
Publikováno v:
Annals of Glaciology. 50:9-16
A number of glaciers in the Canadian High Arctic are composed primarily of cold ice, but the ice at or near their beds reaches the pressure-melting point (PMP) in the ablation zone. Past modelling studies have suggested that the basal temperatures of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c0961791b0d3861ff82f74f877a323f
https://doi.org/10.3189/172756409789624210
https://doi.org/10.3189/172756409789624210
Publikováno v:
Scopus-Elsevier
Mair, D, Nienow, P, Sharp, M, Wohlleben, T & Willis, I 2002, ' Influence of subglacial drainage system evolution on glacier surface motion: Haut Glacier d'Arolla, Switzerland ', Journal of Geophysical Research, vol. 107, no. B8, EPM 8, pp. 1-13 . https://doi.org/10.1029/2001JB000514
Mair, D, Nienow, P, Sharp, M, Wohlleben, T & Willis, I 2002, ' Influence of subglacial drainage system evolution on glacier surface motion: Haut Glacier d'Arolla, Switzerland ', Journal of Geophysical Research, vol. 107, no. B8, EPM 8, pp. 1-13 . https://doi.org/10.1029/2001JB000514
[1] The relationship between the evolution of subglacial drainage system morphology and spatial patterns of glacier surface velocity was investigated using dye tracing experiments and ground surveying throughout the 1995 melt season at Haut Glacier d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::67386a0d5a5e93ad8b7b70bc4dff7415
https://doi.org/10.1029/2001jb000514
https://doi.org/10.1029/2001jb000514