Zobrazeno 1 - 10
of 147
pro vyhledávání: '"Livingstone, S.J."'
Autor:
Rex, C.L., Bateman, M.D., Buckland, P.C., Panagiotakopulu, E., Livingstone, S.J., Hardiman, M., Eddey, L.
Publikováno v:
In Quaternary Science Reviews 1 January 2023 299
Autor:
Davies, B.J., Livingstone, S.J., Roberts, D.H., Evans, D.J.A., Gheorghiu, D.M., Ó Cofaigh, C.
Publikováno v:
In Quaternary Science Reviews 1 December 2019 225
Publikováno v:
In Quaternary Science Reviews 15 September 2016 148:128-145
Autor:
Hornsey, J., Rowan, A.V., Kirkbride, M.P., Livingstone, S.J., Fabel, D., Rodes, A., Quincey, D.J., Hubbard, B., Jomelli, V.
The dynamic response of large mountain glaciers to climatic forcing operates over timescales of several centuries and therefore understanding how these glaciers change requires observations of their behavior through the Holocene. We used Be-10 exposu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::1665d9030dae549e6beb5e099283c4bf
Publikováno v:
Journal of Maps
Subglacial drainage systems are crucial elements of glaciers and ice sheets because they modulate ice\ud flow velocity. However, logistical challenges of measuring subglacial processes beneath contemporary\ud ice and natural limitations in long-term
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::d89ad3fdcca810b1ff8401809752627e
https://eprints.whiterose.ac.uk/185721/7/17445647.2022.pdf
https://eprints.whiterose.ac.uk/185721/7/17445647.2022.pdf
Eskers are primarily ridges of glaciofluvial sediment deposited in subglacial, englacial and supraglacial conduits. They are\ud typically straight to sinuous features, however, their planform morphology can be highly diverse. Esker enlargements\ud ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::9e0aeefd58ac6da17009aee7f1e6255c
https://eprints.whiterose.ac.uk/177182/1/Dewald_etal_EskerEnlargements_final.pdf
https://eprints.whiterose.ac.uk/177182/1/Dewald_etal_EskerEnlargements_final.pdf
Akademický článek
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The Polish sector of the last Scandinavian Ice Sheet is a key area for studying ice‐sheet drainage and decay from its local Last Glacial Maximum (LGM) extent, as it is located at the terrestrial terminus of the large and dynamic Baltic Ice Stream C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::06265eb1e9f9b9532bf039938ea1f4f5
https://eprints.whiterose.ac.uk/169892/1/Szuman2021_DynamicsSIS_preprint.pdf
https://eprints.whiterose.ac.uk/169892/1/Szuman2021_DynamicsSIS_preprint.pdf
Autor:
Vérité, J., Ravier, É., Bourgeois, O., Bessin, P., Livingstone, S.J., Clark, C.D., Pochat, S., Mourgues, R.
Publikováno v:
SSRN Electronic Journal.
Fluctuations in meltwater discharge below modern glaciers and ice sheets due to diurnal, seasonal and long-term temperature variations are modulated by complex interactions between subglacial drainage, basal processes and bedform development. The bed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3607f6c20588133d31d293ee177d481e
https://doi.org/10.2139/ssrn.3978870
https://doi.org/10.2139/ssrn.3978870