Synthesis of all areas
During the course of the project, Area S will use the results (e.g. new parameterizations or refined model set ups) of the other areas in the projects to further enhance and improve climate models.
Xu, J., Koldunov, N. V., Remedio, A.R.C., Sein, D.V., Zhi, X., Jiang, X., Xu, M., Zhu, X., Fraedrich, K., Jacob, D. (2018). On the role of horizontal resolution over the Tibetan Plateau in the REMO regional climate model, Climate Dynamics, February 8, 2018, 1–18, https://doi.org/10.1007/s00382-018-4085-7
Sein, D. V., Koldunov, N. V., Danilov, S., Wang, Q., Sidorenko, D., Fast, I., ... and Jung, T. (2017). Ocean modeling on a mesh with resolution following the local Rossby radius. Journal of Advances in Modeling Earth Systems, 9(7), 2601-2614.
Koldunov, N., Köhl, A., Serra, N., and Stammer, D. (2017). Sea ice assimilation into a coupled ocean–sea ice model using its adjoint. Cryosphere, 11, 2265-2281.