MPAS Data Assimilation


Data assimilation for MPAS is available as an ensemble Kalman filter (EnKF) implemented through Data Assimilation Research Testbed (DART). This work is done in a collaborative effort between the Mesoscale and Microscale Meteorology (MMM) Division and the DART development team in the Institute for Mathematics Applied to Geosciences (IMAGe) in the National Center for Atmospheric Research (NCAR).

The latest official release of DART (the "Lanai" version) includes interfaces for both MPAS-Atmosphere and MPAS-Ocean. To download the code, click here or email dart at ucar dot edu.

In collaboration with NOAA's Earth System Research Laboratory, related efforts are also underway to explore ensemble data assimilation for MPAS-Atmosphere with the Gridpoint Statistical Interpolation (GSI) scheme that is operational at the National Centers for Environmental Prediction. Further collaborations related to MPAS data assimilation are welcome (see contact information below).

Spaghetti diagram of the ensemble analysis in terms of geopotential height at 500 mb valid at 12Z 5 Dec 2008.

The MPAS/DART interface

The interface is built on MPAS's unstructured centroidal Voronoi mesh, and does not regrid to latitude-longitude grids. In MPAS, the finite-volume approach based on a C-grid staggering retains prognostic equations for mass at the center of finite-volume cells and for the normal component of velocity (u) at the faces (or edges in 2D) of the cells. The normal component of velocity (u) at cell edges is then used to reconstruct zonal and meridional winds at cell centers () using radial basis functions (RBFs).

To avoid the singularity issue on the poles, the cartesian coordinate is employed.

The forward operators on the unstructured grid mesh are constructed as follows.
The dual of the Voronoi mesh, or the triangular mesh (shown as dashed lines in the figure to the right), is used to search the closest cell center to an arbitrary (or observation) point, then find three cell centers of the triangle enclosing the desired point. Mass fields are then horizontally interpolated from the cell centers to the observation location using a barycentric (e.g., area-weighted) interpolation.
While the observed wind quantities are zonal and meridional winds, the normal component of velocity (u) is the only prognostic wind variable in MPAS, we thus implement a couple of different ways of assimilating wind observations. The options determine which wind variables are used in the forward operator to compute expected observation values; how the horizontal interpolation is computed in that forward operator; and how the assimilation increments are applied to update the wind quantities in the state vector of the analysis.
Preliminary results based on real data assimilation experiments indicate that performance is better when the zonal and meridional winds are used as input to the forward operator that uses Barycentric interpolation and the prognostic u wind is incrementally updated. However, there remain scientific questions about how best to handle the wind fields under different situations. For the details on the wind data strategy, refer to the documentation in DART.

Grid structure used in the MPAS/DART interface

For any questions or future collaboration, please contact either So-Young Ha ( or Chris Snyder (