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pro vyhledávání: '"Brisbourne, AM"'
Autor:
O'Donnell, JP, Brisbourne, AM, Stuart, GW, Dunham, CK, Yang, Y, Nield, GA, Whitehouse, PL, Nyblade, AA, Wiens, DA, Aster, RC, Anandakrishnan, S, Huerta, AD, Wilson, T, Winberry, JP
Using 8‐ to 25‐s‐period Rayleigh and Love wave phase velocity dispersion data extracted from seismic ambient noise, we (i) model the 3‐D shear wave velocity structure of the West Antarctic crust and (ii) map variations in crustal radial aniso
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::ee3658d85e0f6c524c0af50fffde591f
https://eprints.whiterose.ac.uk/155266/1/O'Donnell_et_al-2019-Geochemistry,_Geophysics,_Geosystems.pdf
https://eprints.whiterose.ac.uk/155266/1/O'Donnell_et_al-2019-Geochemistry,_Geophysics,_Geosystems.pdf
Autor:
Brisbourne, AM, Smith, AM, Vaughan, DG, King, EC, Davies, D, Bingham, RG, Smith, EC, Nias, IJ, Rosier, SHR
Publikováno v:
Brisbourne, A M, Smith, A M, Vaughan, D G, King, E C, Davies, D, Bingham, R G, Smith, E C, Nias, I & Rosier, S H R 2017, ' Bed conditions of Pine Island Glacier, West Antarctica ', Journal of Geophysical Research: Earth Surface . https://doi.org/10.1002/2016JF004033
Journal of Geophysical Research: Earth Surface
Journal of Geophysical Research: Earth Surface
Although 90% of Antarctica's discharge occurs via its fast-flowing ice streams, our ability to project future ice-sheet response has been limited by poor observational constraints on the ice-bed conditions used in numerical models to determine basal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0b3c1a442ed3ab1a3f9a943ddca011ff
Wiley Online Library
Wiley Online Library
Improving our understanding of glacial sliding is crucial for constraining basal drag in ice dynamics models. We use icequakes, sudden releases of seismic energy as the ice slides over the bed, to provide geophysical observations that can be used to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::736005ff9cfbd39c2e6fcb2a144612ac
Icequakes at or near the bed of a glacier have the potential to allow us to investigate the interaction of ice with the underlying till or bedrock. Understanding this interaction is important for studying basal sliding of glaciers and ice streams, a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c1a6c7fa302569f28c5dc77e25e5ecbc
Akademický článek
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Publikováno v:
Journal of Geophysical Research: Earth Surface, 125 (11)
Improving our understanding of glacial sliding is crucial for constraining basal drag in ice dynamics models. We use icequakes, sudden releases of seismic energy as the ice slides over the bed, to provide geophysical observations that can be used to
Autor:
Bingham RG; School of GeoSciences, University of Edinburgh, Edinburgh, EH8 9XP, UK. r.bingham@ed.ac.uk., Vaughan DG; British Antarctic Survey, Cambridge, CB3 0ET, UK., King EC; British Antarctic Survey, Cambridge, CB3 0ET, UK., Davies D; School of GeoSciences, University of Edinburgh, Edinburgh, EH8 9XP, UK., Cornford SL; Department of Geography, College of Science, Swansea University, Swansea, SA2 8PP, UK., Smith AM; British Antarctic Survey, Cambridge, CB3 0ET, UK., Arthern RJ; British Antarctic Survey, Cambridge, CB3 0ET, UK., Brisbourne AM; British Antarctic Survey, Cambridge, CB3 0ET, UK., De Rydt J; British Antarctic Survey, Cambridge, CB3 0ET, UK., Graham AGC; College of Life and Environmental Sciences, University of Exeter, Exeter, EX4 4RJ, UK., Spagnolo M; School of Geosciences, University of Aberdeen, Aberdeen, AB24 3UF, UK.; Department of Earth and Planetary Science, University of California, Berkeley, CA 94720-4767, USA., Marsh OJ; Gateway Antarctica, University of Canterbury, Christchurch 8140, New Zealand., Shean DE; Applied Physics Laboratory, University of Washington, Seattle, WA 98105-6698, USA.
Publikováno v:
Nature communications [Nat Commun] 2017 Nov 20; Vol. 8 (1), pp. 1618. Date of Electronic Publication: 2017 Nov 20.