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The disintegration of the eastern Antarctic Peninsula’s Larsen A and B ice shelves has been attributed to atmosphere and ocean warming, and increased mass-losses from the glaciers once restrained by these ice shelves have increased Antarctica’s t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7a3c87f70f58bf071d721a1c26974cda
https://www.repository.cam.ac.uk/handle/1810/336954
https://www.repository.cam.ac.uk/handle/1810/336954
Major glaciations or ‘ice ages’ are known to have affected the Earth's surface over the past three billion years. The best preserved records of these glaciations are often found in high-latitude continental margin settings where sediment has been
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::88bcf680004d8fe6e7d8d740140c8218
Autor:
Batchelor CL; School of Geography, Politics and Sociology, Newcastle University, Newcastle upon Tyne, UK. christine.batchelor@ncl.ac.uk., Christie FDW; Scott Polar Research Institute, University of Cambridge, Cambridge, UK., Ottesen D; Geological Survey of Norway, Trondheim, Norway., Montelli A; Scott Polar Research Institute, University of Cambridge, Cambridge, UK., Evans J; Geography and Environment, School of Social Sciences and Humanities, Loughborough University, Loughborough, UK., Dowdeswell EK; Scott Polar Research Institute, University of Cambridge, Cambridge, UK., Bjarnadóttir LR; Geological Survey of Norway, Trondheim, Norway., Dowdeswell JA; Scott Polar Research Institute, University of Cambridge, Cambridge, UK.
Publikováno v:
Nature [Nature] 2023 May; Vol. 617 (7959), pp. 105-110. Date of Electronic Publication: 2023 Apr 05.
Knowledge of the past behavior of the outlet glaciers of Southeast (SE) Greenland is necessary to understand and model spatial differences in the response of the Greenland Ice Sheet (GIS) to climatic changes. Here we use bathymetric data to map the d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bda6f3359b5580e7bcc885cf9dad455b
https://www.repository.cam.ac.uk/handle/1810/290940
https://www.repository.cam.ac.uk/handle/1810/290940
Autor:
Kirkham, JD, Hogan, KA, Larter, RD, Arnold, NS, Nitsche, FO, Kuhn, G, Gohl, K, Anderson, JB, Dowdeswell, JA
© 2020 The Authors Expanding multibeam bathymetric data coverage over the last two decades has revealed extensive networks of submarine channels incised into bedrock on the Antarctic inner continental shelf. The large dimensions and prevalence of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9e30fd1103398bc6b16bcbb321f1d4ff
Autor:
Batchelor, CL, Montelli, A, Ottesen, D, Evans, J, Dowdeswell, EK, Christie, FDW, Dowdeswell, JA
Autonomous Underwater Vehicles (AUVs) deployed close to the seafloor can acquire high-resolution geophysical data about the topography and shallow stratigraphy of the seabed, yet have had limited application within the fields of glacial geomorphology
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c9b90e84e8e87d8ad92a19aaec19c55e
https://www.repository.cam.ac.uk/handle/1810/311199
https://www.repository.cam.ac.uk/handle/1810/311199
Autor:
Dowdeswell, JA, Batchelor, CL, Dorschel, B, Benham, TJ, Christie, FDW, Dowdeswell, EK, Montelli, A, Arndt, JE, Gebhardt, C
Marine-geophysical evidence on sea-floor morphology and shallow acoustic stratigraphy are used to examine the substrate around the location at which Sir Ernest Shackleton's ship Endurance sank in 1915 and on the continental slope-shelf sedimentary sy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5a7d60c5b4e48d24512a3144e8fe4ad6
https://www.repository.cam.ac.uk/handle/1810/305656
https://www.repository.cam.ac.uk/handle/1810/305656