• Arctic Amplification of Precipitation Changes—The Energy Hypothesis 

      Pithan, FelixORCIDiD; Jung, ThomasORCIDiD (Geophysical Research Letters, 2021-11-06)
      Temperature and precipitation change more strongly in the Arctic than at lower latitudes, with central Arctic boreal winter precipitation projected to double in the 21st century in a high‐emission scenario. This enhanced ...
    • Clouds, radiation, and atmospheric circulation in the present‐day climate and under climate change 

      Voigt, AikoORCIDiD; Albern, Nicole; Ceppi, PauloORCIDiD; Grise, KevinORCIDiD; Li, Ying; Medeiros, BrianORCIDiD (Wiley Interdisciplinary Reviews: Climate Change, 2020-11-25)
      By interacting with radiation, clouds modulate the flow of energy through the Earth system, the circulation of the atmosphere, and regional climate. We review the impact of cloud‐radiation interactions for the atmospheric ...
    • Comparing the Properties of ICME-Induced Forbush Decreases at Earth and Mars 

      Freiherr von Forstner, Johan L.ORCIDiD; Guo, JingnanORCIDiD; Wimmer-Schweingruber, Robert F.ORCIDiD; Dumbovic, Mateja; Janvier, Miho; Démoulin, PascalORCIDiD; Veronig, AstridORCIDiD; Temmer, ManuelaORCIDiD; Papaioannou, Athanasios; Dasso, Sergio; Hassler, Donald M.ORCIDiD; Zeitlin, Cary J.ORCIDiD (Journal of Geophysical Research: Space Physics, 2020)
      Forbush decreases (FDs), which are short-term drops in the flux of galactic cosmic rays, are caused by the shielding from strong and/or turbulent magnetic structures in the solar wind, especially interplanetary coronal ...
    • No Cookie for Climate Change 

      Voigt, A.; Albern, N. (Geophysical Research Letters, 2019)
      Climate change leads to changes in cloud-radiative heating, which previous work showed have a substantial impact on the response of the atmospheric circulation to climate change. We here compare to what extent this ...