• Eddy Kinetic Energy in the Arctic Ocean From a Global Simulation With a 1-km Arctic 

      Wang, QiangORCIDiD; Koldunov, Nikolay V.ORCIDiD; Danilov, SergeyORCIDiD; Sidorenko, DmitryORCIDiD; Wekerle, ClaudiaORCIDiD; Scholz, PatrickORCIDiD; Bashmachnikov, Igor L.ORCIDiD; Jung, ThomasORCIDiD (Geophysical Research Letters, 2020)
      Simulating Arctic Ocean mesoscale eddies in ocean circulation models presents a great challenge because of their small size. This study employs an unstructured-mesh ocean-sea ice model to conduct a decadal-scale global ...
    • Fast EVP Solutions in a High-Resolution Sea Ice Model 

      Koldunov, Nikolay V.ORCIDiD; Danilov, SergeyORCIDiD; Sidorenko, DmitryORCIDiD; Hutter, NilsORCIDiD; Losch, MartinORCIDiD; Goessling, HelgeORCIDiD; Rakowsky, NataljaORCIDiD; Scholz, PatrickORCIDiD; Sein, DmitryORCIDiD; Wang, QiangORCIDiD; Jung, ThomasORCIDiD (Journal of Advances in Modeling Earth Systems, 2019)
      Sea ice dynamics determine the drift and deformation of sea ice. Nonlinear physics, usually expressed in a viscous-plastic rheology, makes the sea ice momentum equations notoriously difficult to solve. At increasing sea ...
    • Ocean Model Formulation Influences Transient Climate Response 

      Semmler, TidoORCIDiD; Jungclaus, JohannORCIDiD; Danek, ChristopherORCIDiD; Goessling, Helge F.ORCIDiD; Koldunov, Nikolay V.ORCIDiD; Rackow, ThomasORCIDiD; Sidorenko, DmitryORCIDiD (Journal of Geophysical Research: Oceans, 2021-12-05)
      The transient climate response (TCR) is 20% higher in the Alfred Wegener Institute Climate Model (AWI‐CM) compared to the Max Planck Institute Earth System Model (MPI‐ESM) whereas the equilibrium climate sensitivity (ECS) ...