Search Results - "DOWDESWELL, JULIAN A."
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Distinctive iceberg ploughmarks on the mid-Norwegian margin: Tidally influenced chains of pits with implications for iceberg drift
Published in Arctic, antarctic, and alpine research (31-12-2022)“…Curvilinear depressions and chains of asymmetrical to circular pits up to a few meters deep and a few tens of meters wide have been mapped on the upper…”
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2
Basal melting of Ross Ice Shelf from solar heat absorption in an ice-front polynya
Published in Nature geoscience (01-06-2019)“…Ice–ocean interactions at the bases of Antarctic ice shelves are rarely observed, yet have a profound influence on ice sheet evolution and stability. Ice sheet…”
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3
The International Bathymetric Chart of the Arctic Ocean (IBCAO) Version 3.0
Published in Geophysical research letters (28-06-2012)“…The International Bathymetric Chart of the Arctic Ocean (IBCAO) released its first gridded bathymetric compilation in 1999. The IBCAO bathymetric portrayals…”
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Anatomy of Heinrich Layer 1 and its role in the last deglaciation
Published in Paleoceanography (01-03-2017)“…X‐ray fluorescence (XRF) core scanning and X‐ray computed tomography data were measured every 1 mm to study the structure of Heinrich Event 1 during the last…”
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The unquantified mass loss of Northern Hemisphere marine-terminating glaciers from 2000–2020
Published in Nature communications (11-10-2022)“…In the Northern Hemisphere, ~1500 glaciers, accounting for 28% of glacierized area outside the Greenland Ice Sheet, terminate in the ocean. Glacier mass loss…”
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Geophysical constraints on the dynamics and retreat of the Barents Sea ice sheet as a paleobenchmark for models of marine ice sheet deglaciation
Published in Reviews of geophysics (1985) (01-12-2015)“…Our understanding of processes relating to the retreat of marine‐based ice sheets, such as the West Antarctic Ice Sheet and tidewater‐terminating glaciers in…”
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Intra- and inter-annual variability in dynamic discharge from the Academy of Sciences Ice Cap, Severnaya Zemlya, Russian Arctic, and its role in modulating mass balance
Published in Journal of glaciology (01-10-2019)“…We determined ice velocities for the Academy of Sciences Ice Cap, Severnaya Zemlya, Russian Arctic, during November 2016–November 2017, by feature-tracking 54…”
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Flow and retreat of the Late Quaternary Pine Island-Thwaites palaeo-ice stream, West Antarctica
Published in Journal of Geophysical Research: Earth Surface (01-09-2010)“…Multibeam swath bathymetry and sub‐bottom profiler data are used to establish constraints on the flow and retreat history of a major palaeo‐ice stream that…”
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9
Geomorphic signature of Antarctic submarine gullies: Implications for continental slope processes
Published in Marine geology (01-03-2013)“…Five quantitatively distinct gully types are identified on the Antarctic continental margin from swath bathymetric data of over 1100 individual features. The…”
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Rapid dynamic activation of a marine-based Arctic ice cap
Published in Geophysical research letters (28-12-2014)“…We use satellite observations to document rapid acceleration and ice loss from a formerly slow‐flowing, marine‐based sector of Austfonna, the largest ice cap…”
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Progress toward globally complete frontal ablation estimates of marine-terminating glaciers
Published in Annals of glaciology (01-09-2022)“…Knowledge of frontal ablation from marine-terminating glaciers (i.e., mass lost at the calving face) is critical for constraining glacier mass balance,…”
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Variability in ice motion and dynamic discharge from Devon Ice Cap, Nunavut, Canada
Published in Journal of glaciology (01-06-2017)“…Feature tracking of approximately annually separated Landsat-7 ETM+ imagery acquired from 1999 to 2010 and speckle tracking of 24-day separated RADARSAT-2…”
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13
Oceanic heat transport onto the Amundsen Sea shelf through a submarine glacial trough
Published in Geophysical research letters (01-01-2007)“…Glaciers which drain the West Antarctic Ice Sheet (WAIS) into the Amundsen Sea are accelerating and thinning rapidly. These observations have been attributed…”
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14
An Arctic Ocean ice shelf during MIS 6 constrained by new geophysical and geological data
Published in Quaternary science reviews (01-12-2010)“…The hypothesis of floating ice shelves covering the Arctic Ocean during glacial periods was developed in the 1970s. In its most extreme form, this theory…”
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Till characteristics, genesis and transport beneath Antarctic paleo-ice streams
Published in Journal of Geophysical Research - Earth Surface (01-09-2007)“…Marine geophysical data from the Antarctic continental shelf indicate the former presence of ice streams that drained through bathymetric troughs during the…”
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Morphology, sedimentary infill and depositional environments of the Early Quaternary North Sea Basin (56°–62°N)
Published in Marine and petroleum geology (01-09-2014)“…The North Sea Basin has been subsiding during the Quaternary and contains hundreds of metres of fill. Seismic surveys (170 000 km2) provide new evidence on…”
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Evolution of subglacial bedforms along a paleo-ice stream, Antarctic Peninsula continental shelf
Published in Geophysical research letters (01-04-2002)“…Geophysical data from the Antarctic Peninsula continental shelf reveal streamlined subglacial bedforms in a cross‐shelf trough. Bedforms exhibit progressive…”
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18
A historical Southern Ocean climate dataset from whaling ships’ logbooks
Published in Geoscience data journal (01-06-2019)“…Historical ship logbooks provide vital historic meteorological observations in the Southern Ocean, one of the largest climate‐data deficient regions on the…”
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Antarctic ice-shelf advance driven by anomalous atmospheric and sea-ice circulation
Published in Nature geoscience (01-05-2022)“…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…”
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Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks
Published in Nature (London) (26-10-2017)“…Plough marks in Pine Island Bay, West Antarctica, left by the keels of drifting icebergs 12,000 years ago provide evidence that marine ice-cliff instability…”
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