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+## Current AMIP components
+
+### Atmosphere
+
+Dynamical core:
+- Equation: non-hydrostatic and fully compressible
+- Prognostic variables: Density, velocity components, total energy, total specific humidity
+- Spatial discretization: Spectral element in the horizontal, finite difference in the vertical, cubed sphere
+- Time stepping: Implicit-explicit additive Runge–Kutta method
+
+Parameterizations:
+
+- Radiation: A scheme based on RRTM for General circulation model applications—Parallel (RRTMGP) (Pincus et al. 2019)
+
+- Convection and turbulence: Diagnostic Eddy-diffusivity Mass-Flux (EDMF) scheme with prognostic turbulent kinetic energy. 
+EDMF is a unified parameterization for turbulence and convection (Tan et al. 2018, Cohen et al. 2020, Lopez-Gomez et al. 2020). The grid is decomposed into convective updrafts and the turbulent environment. 
+Updraft properties are calculated from mass, momentum and energy conservation of the updraft. 
+Mass and momentum exchange between the updrafts and the environment, and
+turbulent mixing in the environment, are represented with physical closures. Currently, only one updraft is used.
+
+- Microphysics: 0-moment scheme, where cloud condensate is removed in-situ with a constant timescale
+
+- Surface fluxes: A scheme based on Monin-Obukhov similarity theory, with constant roughness lengths over land and ocean
+
+- Orographic gravity wave drag: None
+
+- Non-orographic gravity wave drag: None
+
+- Aerosols and chemistry: None
+
+### Land
+
+Dynamical core:
+- Equation: Following Manabe bucket hydrology scheme (Manabe 1969)
+- Prognostic variables: Temperature, water content, snow water content
+- Spatial discretization: Finite difference, multiple independent columns on the sphere
+- Time stepping: Explicit additive Runge–Kutta method
+
+Land surface albedo: 
+- Bare ground: Prescribed from files
+- Snow: Constant
+
+### Sea ice
+
+Thermodynamics: 0-layer model, with prognostic ice surface temperature and fixed ice thickness
+
+### Coupling
+
+Sequential coupling. Fluxes over a heterogeneous surface are calculated using the averaged surface properties.
+
+## References
+
+[Manabe 1969](https://journals.ametsoc.org/view/journals/mwre/97/11/1520-0493_1969_097_0739_catoc_2_3_co_2.xml): Climate and ocean circulation. I. The atmospheric circulation and the hydrology of the earth's surface.
+
+[Pincus et al. 2019](https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2019MS001621): Balancing Accuracy, Efficiency, and Flexibility in Radiation Calculations for Dynamical Models
+
+[Tan et al. 2018](https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2017MS001162): An Extended Eddy-Diffusivity Mass-Flux Scheme for Unified Representation of Subgrid-Scale Turbulence and Convection
+
+[Cohen et al. 2020](https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020MS002162): Unified Entrainment and Detrainment Closures for Extended Eddy-Diffusivity Mass-Flux Schemes
+
+[Lopez-Gomez et al. 2020](https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020MS002161): A Generalized Mixing Length Closure for Eddy-Diffusivity Mass-Flux Schemes of Turbulence and Convection
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