Results 181 to 190 of about 43,823 (313)
Movement of the Ward Hunt Ice Shelf, Ellesmere Island, N.W.T., Canada [PDF]
Egon Dorrer
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Glacier evolution and environmental changes in the northern Jan‐Mayen from the early deglaciation and well into the Holocene are discussed. Results are based on a large chronological dataset (TCN and radiocarbon dates), integrated with field data on glacial landforms and sediments, including the use of GPR.
Astrid Lyså+5 more
wiley +1 more source
Lipid Biomarkers From Microbial Mats on the McMurdo Ice Shelf, Antarctica: Signatures for Life in the Cryosphere. [PDF]
Evans TW+8 more
europepmc +1 more source
Studies of Ice Movements on the Ward Hunt Ice Shelf by Means of Triangulation-Trilateration
Gottfried Konecny, Wolfgang Faig
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Sediments Exposed on the Surface of the Ross Ice Shelf, Antarctica [PDF]
David R. Gaylord, J. David Robertson
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Reconstructions of the maximum extent of the Laurentide Ice Sheet (LIS) and its associated ice flows at the Last Glacial Maximum (LGM) are needed for understanding how marine‐based ice sheets will respond to modern climate change. Here, we provide evidence for the location of the maximal extent of the LIS margin during the LGM in Merchants and ...
Alexis P. Belko+4 more
wiley +1 more source
High spatial and temporal variability in Antarctic ice discharge linked to ice shelf buttressing and bed geometry. [PDF]
Miles BWJ+5 more
europepmc +1 more source
Modelling the three-dimensional, diagnostic anisotropy field of an ice rise [PDF]
Polar ice develops anisotropic crystal orientation fabrics under deformation, yet ice is most often modelled as an isotropic fluid. We present three-dimensional simulations of the crystal orientation fabric of Derwael Ice Rise including the surrounding ice shelf using a crystal orientation tensor evolution equation corresponding to a fixed velocity ...
arxiv
Glaciological and Oceanographic Calculations of the Mass Balance and Oxygen Isotope Ratio of a Melting Ice Shelf [PDF]
J. R. Potter, J. G. Paren, J. Loynes
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We have mapped a 60 km long, 30 km wide, 120 m deep buried glacially eroded trough on the North Sea Plateau, west of the Norwegian Channel (59°N, 3°E). The trough was carved out by an ice stream that flowed out from western Norway and crossed the Norwegian Channel in a southwestern direction during the penultimate or Saalian glaciation.
Dag Ottesen+4 more
wiley +1 more source