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Summary

First release of version 2 of the Energy Exascale Earthy System Model contains the following changes from v1.0

EAM

The atmosphere component remains EAM. Major changes since version 1 include: all column-physics parameterizations are computed on a separate grid that has approximately half the number of points of the dynamics grid, a new nonhydrostatic dynamical core (running in hydrostatic mode) with semi-Lagrangian tracer transport, CLUBB has been changed from v1 to v2,

ELM

The land component is still ELM. Major changes since version 1 include: …

General MPAS improvements

MPAS still provides the components for ocean, sea-ice and land-ice.

MPAS-Ocean

  • Redi isopycnal mixing has been updated, tested, and tuned in combination with the Gent-McWilliams parameterization.

  • A new semi-implicit barotropic solver has been introduced as an option.

  • There have been a number of performance improvements, including an initial GPU port of several portions of the model using OpenACC directives.

  • Ability to have inactive top cells below ice shelves.

  • Tracking and verification of flux budgets with coupler

  • Improvements in code simplicity and readability include transplanting MPAS code directly into E3SM repository, direct access to mesh and config variables, and excluding init mode in forward runs.

  • Addition of tidal forcing, wetting and drying for shorelines, internal wave drag, GOTM vertical mixing library, and sediment transport (all not yet fully validated).

MPAS-seaice

The sea-ice component remains MPAS-seaice. Major changes since version 1 include:…

MPAS-Albany-landice

The land-ice component remains MPAS-Albany-landice and is a static ice sheet. Major changes since version 1 include preparation for using an active ice sheet such as:

  • MALI code was moved from a submodule to instead exist directly within the E3SM repository.

  • An ice shelf damage evolution scheme was added, but is not yet coupled to calving or advection.

  • A von Mises tensile stress calving schemes was implemented and the calving algorithm was rewritten to eliminate a number of bugs.

  • The grounded marine terminus ocean melting scheme from ISMIP6-Greenland was implemented.

  • The option to use a regularized Coulomb basal friction law and a general power law basal friction law were added.

  • The sub-ice-shelf melting scheme from ISMIP6-Antarctica was added.

  • The prescribed mask-calving forcing scheme from ISMIP6-Antarctica was added.

Coupler/Configurations

All components allow regional refinement of their meshes and an example of refinement in and around North America is provided.

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