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## Current AMIP components | ||
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### Atmosphere | ||
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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 | ||
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Parameterizations: | ||
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- Radiation: A scheme based on RRTM for General circulation model applications—Parallel (RRTMGP) (Pincus et al. 2019) | ||
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- 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. | ||
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- Microphysics: 0-moment scheme, where cloud condensate is removed in-situ with a constant timescale | ||
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- Surface fluxes: A scheme based on Monin-Obukhov similarity theory, with constant roughness lengths over land and ocean | ||
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- Orographic gravity wave drag: None | ||
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- Non-orographic gravity wave drag: None | ||
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- Aerosols and chemistry: None | ||
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### Land | ||
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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 | ||
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Land surface albedo: | ||
- Bare ground: Prescribed from files | ||
- Snow: Constant | ||
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### Sea ice | ||
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Thermodynamics: 0-layer model, with prognostic ice surface temperature and fixed ice thickness | ||
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### Coupling | ||
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Sequential coupling. Fluxes over a heterogeneous surface are calculated using the averaged surface properties. | ||
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## References | ||
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[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. | ||
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[Pincus et al. 2019](https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2019MS001621): Balancing Accuracy, Efficiency, and Flexibility in Radiation Calculations for Dynamical Models | ||
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[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 | ||
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[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 | ||
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[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 |