• Seasonal phytoplankton blooms in the North Atlantic linked to the overwintering strategies of copepods 

      Friedland, Kevin D; Record, Nicholas R; Asch, Rebecca G; Kristiansen, Trond; Saba, Vincent S; Drinkwater, Kennneth F.; Henson, Stephanie; Leaf, Robert T; Morse, Ryan E; Johns, David G; Large, Scott I; Hjøllo, Solfrid Sætre; Nye, Janet A; Alexander, Mike A; Ji, Rubao (Journal article; Peer reviewed, 2016)
      The North Atlantic Ocean contains diverse patterns of seasonal phytoplankton blooms with distinct internal dynamics. We analyzed blooms using remotely-sensed chlorophyll a concentration data and change point statistics. ...
    • The importance of calibrating climate change projections to local conditions at aquaculture sites 

      Falconer, Lynne; Hjøllo, Solfrid Sætre; Telfer, Trevor C.; McAdam, Bruce J.; Hermansen, Øystein; Ytteborg, Elisabeth (Peer reviewed; Journal article, 2020)
      Future climate projections are usually only available at global or coarse scale and the focus is often on long-term global or regional averages. Though useful to analyse general trends and identify potential risks and ...
    • Transportation and predation control structures the distribution of a key calanoid in the Nordic Seas 

      Aarflot, Johanna Myrseth; Hjøllo, Solfrid Sætre; Strand, Espen; Skogen, Morten D. (Peer reviewed; Journal article, 2022)
      The largest Calanus species in the Nordic Seas is also the copepod for which we have the poorest knowledge. Recent studies have shown that C. hyperboreus is more likely of sub-Arctic rather than Arctic origins, and the ...
    • Why do regional biogeochemical models produce contrasting future projections of primary production in the Barents Sea? 

      Mousing, Erik Askov; Ellingsen, Ingrid Helene; Hjøllo, Solfrid Sætre; Husson, Berengere; Skogen, Morten D.; Wallhead, Philip (Peer reviewed; Journal article, 2023)
      Projected future changes in primary production in the Barents Sea vary among different regional biogeochemical models, with some showing an increase, some a decrease, and some no change. This variability has been attributed ...