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Fletta eftir höfundi "Brynjólfsson, Skafti"

Fletta eftir höfundi "Brynjólfsson, Skafti"

Röðun: Raða: Niðurstöður:

  • Benediktsson, Ívar Örn; Aradóttir, Nína; Ingólfsson, Ólafur; Brynjólfsson, Skafti (Elsevier, 2022-01)
    Ice streams are thought to have regulated the past Iceland Ice Sheet (IIS) during and following the Last Glacial Maximum (LGM) by discharging ice and sediment from the interior of the ice sheet towards the shelf edge. Previous assessments of ice streams ...
  • Brynjólfsson, Skafti (Norwegian University of Science and Technology; University of Iceland, 2015-09)
    This thesis describes the glacial history, glacier dynamics, sediments and landforms of the Drangajökull ice cap as well as the glacial history and dynamics of the eastern Vestfirðir peninsula in northwest Iceland from the Late Weichselian until present. ...
  • Allaart, Lis; Schomacker, Anders; Håkansson, Lena M.; Farnsworth, Wesley Randall; Brynjólfsson, Skafti; Grumstad, Andreas; Kjellman, Sofia E. (2021-06-01)
    Climate change is amplified in the Arctic, and establishing baseline data for its current character is important. Here we present a map of the geomorphology of the Femmilsjøen area, Spitsbergen, northern Svalbard. The regional physiography is characterised ...
  • Allaart, Lis; Schomacker, Anders; Larsen, Nicolaj K.; Nørmark, Egon; Rydningen, Tom Arne; Farnsworth, Wesley Randall; Retelle, Michael; Brynjólfsson, Skafti; Forwick, Matthias; Kjellman, Sofia E. (2021-01-01)
    The response of glaciers and ice caps to past climate change provides important insight into how they will react to ongoing and future global warming. In Svalbard, the Holocene glacial history has been studied for many cirque and valley glaciers. ...
  • Kjellman, Sofia E.; Schomacker, Anders; Thomas, Elizabeth K.; Håkansson, Lena; Duboscq, Sandrine; Cluett, Allison A.; Farnsworth, Wesley; Allaart, Lis; Cowling, Owen C.; McKay, Nicholas P.; Brynjólfsson, Skafti; Ingolfsson, Olafur (Elsevier BV, 2020-07-15)
    Arctic precipitation is predicted to increase in the coming century, due to a combination of enhanced northward atmospheric moisture transport and local surface evaporation from ice-free seas. However, large model uncertainties, limited long-term ...