Now showing items 1-3 of 3

    • Effects of CO2 and Ocean Mixing on Miocene and Pliocene Temperature Gradients 

      Lohmann, GerritORCIDiD; Knorr, GregorORCIDiD; Hossain, AkilORCIDiD; Stepanek, ChristianORCIDiD (Paleoceanography and Paleoclimatology, 2022-02-11)
      Cenozoic climate changes have been linked to tectonic activity and variations in atmospheric CO2 concentrations. Here, we present Miocene and Pliocene sensitivity experiments performed with the climate model COSMOS. The ...
    • 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) ...
    • Winter Vertical Diffusion Rates in the Arctic Ocean, Estimated From 7Be Measurements and Dissipation Rate Profiles 

      Schulz, K.ORCIDiD; Kadko, D.ORCIDiD; Mohrholz, V.ORCIDiD; Stephens, M.ORCIDiD; Fer, I.ORCIDiD (Journal of Geophysical Research: Oceans, 2023-02-14)
      Ocean turbulent mixing is a key process affecting the uptake and redistribution of heat, carbon, nutrients, oxygen and other dissolved gasses. Vertical turbulent diffusivity sets the rates of water mass transformations and ...