• Deep weakly-stratified layers in the Greenland Sea 

      Horrach Pou, Joan Mateu (Master thesis, 2021-12-06)
      Deep weakly-stratified layers in the Greenland Sea constitute a mode of convection poorly understood. The Greenland Sea is where the densest portion of the overflow waters on either side of Iceland are formed through ...
    • Thunderstorms in Norway. A climatological and a case study 

      Granerød, Martin (Master thesis, 2011-06-01)
      The object of this thesis are thunderstorms in Norway. In the first part, the variability of thunderstorms in time and space is investigated, based on synoptic observations from 60 weather stations in Norway. An analysis ...
    • Water mass transformation in the Greenland Sea during the period 1986-2016 

      Brakstad, Ailin; Våge, Kjetil; Håvik, Lisbeth; Moore, G.W.K. (Peer reviewed; Journal article, 2019-01)
      Hydrographic measurements from ships, autonomous profiling floats, and instrumented seals over the period 1986–2016 are used to examine the temporal variability in open-ocean convection in the Greenland Sea during winter. ...