Model Description ================= qgs is a Python implementation of an atmospheric model for midlatitudes. It models the dynamics of a 2-layer `quasi-geostrophic`_ (QG) channel atmosphere on a `beta-plane`_, coupled to a simple land or `shallow-water`_ ocean component. It currently has three main modes of operation: * A QG atmosphere coupled to a land surface with topography through friction and with a simple thermal relaxation toward a climatological temperature. See :ref:`files/model/oro_model:Model with an orography and a temperature profile` for a description of this model version. It is also described in detail in the following articles: * Reinhold, B. B., & Pierrehumbert, R. T. (1982). *Dynamics of weather regimes: Quasi-stationary waves and blocking*. Monthly Weather Review, **110** (9), 1105-1145. `doi:10.1175/1520-0493(1982)110%3C1105:DOWRQS%3E2.0.CO;2 `_ * Cehelsky, P., & Tung, K. K. (1987). *Theories of multiple equilibria and weather regimes—A critical reexamination. Part II: Baroclinic two-layer models*. Journal of the atmospheric sciences, **44** (21), 3282-3303. `doi:10.1175/1520-0469(1987)044%3C3282%3ATOMEAW%3E2.0.CO%3B2 `_ * A QG atmosphere coupled to a closed-basin shallow-water ocean through friction and heat exchanges. This configuration is the model `MAOOAM`_ by De Cruz, Demaeyer and Vannitsem. This model exhibits low-frequency variability in a coupled ocean-atmosphere mode. See :ref:`files/model/maooam_model:Coupled ocean-atmosphere model (MAOOAM)` for a description of this model version. It is also described in detail in the articles: * Vannitsem, S., Demaeyer, J., De Cruz, L., & Ghil, M. (2015). *Low-frequency variability and heat transport in a low-order nonlinear coupled ocean–atmosphere model*. Physica D: Nonlinear Phenomena, **309**, 71-85. `doi:10.1016/j.physd.2015.07.006 `_ * De Cruz, L., Demaeyer, J. and Vannitsem, S. (2016). *The Modular Arbitrary-Order Ocean-Atmosphere Model: MAOOAM v1.0*, Geosci. Model Dev., **9**, 2793-2808. `doi:10.5194/gmd-9-2793-2016 `_ * A QG atmosphere coupled to a land surface with topography through friction and heat exchanges. See :ref:`files/model/li_model:Model with an orography and heat exchanges` for a description of this model version. It is also described in detail in the following article: * Li, D., He, Y., Huang, J., Bi, L., & Ding, L. (2018). *Multiple equilibria in a land–atmosphere coupled system.* Journal of Meteorological Research, **32** (6), 950-973. `doi:10.1007/s13351-018-8012-y `_ The shallow-water ocean can in principle be used as a stand-alone model, but this is not implemented for the moment. The modes over which the equations are projected can be modified, leading to other model version. See :ref:`files/examples/VSPD:Recovering the result of Vannitsem, Solé-Pomies and De Cruz (2019)` for an example. More developments are yet to come, see the :ref:`files/general_information:Forthcoming developments` section. Components description ---------------------- .. toctree:: :maxdepth: 2 model/atmosphere model/ocean Model versions description -------------------------- .. toctree:: :maxdepth: 2 model/oro_model model/maooam_model model/li_model .. _quasi-geostrophic: https://en.wikipedia.org/wiki/Quasi-geostrophic_equations .. _shallow-water: https://en.wikipedia.org/wiki/Shallow_water_equations .. _MAOOAM: https://github.com/Climdyn/MAOOAM .. _beta-plane: https://en.wikipedia.org/wiki/Beta_plane