• Arctic Ocean 2022 cruise report 

      Dodd, Paul A.; Nikolopoulos, Anna; Buckley, Shelby; Campbell, Karley; Divine, Dmitry; Eggen, Victoria; Gonçalves-Araujo, Rafael; Granskog, Mats; Hop, Haakon; Kern, Yannick; Koenig, Zoe; Lange, Benjamin A,; Lenss, Megan; Misund, Ole Arve; Muilwijk, Morven; Osanen, Janina; Raffel, Bonnie; Siddarthan, Venkatachalam; Sandven, Håkon; Shereef, Ahammed; Stürzinger, Vegard; Torre, Pedro de la; Fransson, Agneta (Report, 2022-08)
    • The Deep Arctic Ocean and Fram Strait in CMIP6 Models 

      Heuzé, Céline; Zanowski, Hannah; Karam, Salar; Muilwijk, Morven (Journal article, 2023)
      Arctic sea ice loss has become a symbol of ongoing climate change, yet climate models still struggle to reproduce it accurately, let alone predict it. A reason for this is the increasingly clear role of the ocean, especially ...
    • Divergence in Climate Model Projections of Future Arctic Atlantification 

      Muilwijk, Morven; Nummelin, Aleksi Henrynpoika; Heuzé, Céline; Polyakov, Igor V.; Zanowski, Hannah; Smedsrud, Lars Henrik (Journal article, 2022)
      The Arctic Ocean is strongly stratified by salinity in the uppermost layers. This stratification is a key attribute of the region as it acts as an effective barrier for the vertical exchanges of Atlantic Water heat, ...
    • An improved radiative forcing scheme for better representation of Arctic under-ice blooms 

      Gao, Yuexin; Zhang, Yang; Chai, Fei; Granskog, Mats; Duarte, Pedro; Assmy, Philipp (Journal article, 2022)
      In the present study, a newly designed radiative forcing scheme, i.e., impulsive radiative forcing scheme (IRFS), is applied in the one-dimensional Regional Ocean Modeling System-Carbon Silicate Nitrate Ecosystem (ROMS-CoSiNE) ...
    • Regime shift in Arctic Ocean sea ice thickness 

      Sumata, Hiroshi; de Steur, Laura; Divine, Dmitry; Granskog, Mats; Gerland, Sebastian (Journal article, 2023)
      Manifestations of climate change are often shown as gradual changes in physical or biogeochemical properties1. Components of the climate system, however, can show stepwise shifts from one regime to another, as a nonlinear ...