AMPS uses WRF ARW version 3.9.1.1, with polar modifications to the released code to better treat the polar environment.
For recent changes, see History.
Vertical Coordinate:
AMPS uses the WRF hybrid vertical coordinate, in which model levels follow the terrain near the surface, and gradually flatten to isobaric levels at higher model levels (target level ETAC = 0.2).
Vertical Grid:
WRF uses a staggered vertical grid on an η (eta) coordinate, with half-η levels defined halfway between full-η levels.
The AMPS configuration features 61 full-η levels and 60 half-η levels, specified as follows:
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Horizontal Grids:
The AMPS configuration features five two-way interactive grids as follows (see Maps):
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Model Input:
Terrain fields are generated from the RAMP2 data set.
Sea Ice fields are obtained from the Near Real-Time SSM/I EASE-Grid Daily Global Ice Concentration and Snow Extent data set.
SST Data are obtained from daily NCEP Global 0.5-degree analyses.
Model initial and boundary conditions are derived from NCEP 0.25-degree GFS model output (6-hourly intervals out to 120 hours).
Data Assimilation:
WRFVAR 3D Variational data assimilation is used.
Hybrid option running since 2016-05-25/12, currently using an ensemble of approximately 15 members in conjunction with the usual BE Stats.
Options (Physics parameterizations, mostly):
For details on these options below, see the Chapter 5 of the WRF ARW Users' Guide.
Long-wave Radiation:
RRTMG Longwave radiation scheme (ra_lw_physics=4), updated every 15 minutes (radt=15).
Short-wave Radiation:
Goddard shortwave radiation scheme (ra_sw_physics=2), updated every 15 minutes (radt=15).
Boundary Layer:
Mellor-Yamada-Janjic (Eta) TKE scheme (bl_pbl_physics=2), updated every time step (bldt=0).
Surface-layer Scheme:
Monin-Obukhov (Janjic Eta) scheme (sf_sfclay_physics=2),
Land-surface Option:
Unified Noah LSM (sf_surface_physics=2),
Microphysics:
WSM 5-class scheme (mp_physics=4)
Cumulus Parameterization:
Kain-Fritsch (new Eta) parameterization (cu_physics=1) on 24- and 8-km grids, updated every time step (cudt=0)
No cumulus parameterizations (cu_physics=0) on 2.67- and 0.89-km grids
Sea-ice:
A fractional sea-ice implementation is used, in which the surface-layer scheme is called twice: first for completely frozen conditions, then for completely open water conditions. The results of these two calls are then weighted by the sea-ice fraction to determine surface fluxes and other terms.
Upper Boundary Condition:
Model top at 10 mb. Vertical velocity damping is applied (w_damping=1) in the top 7.5 km (zdamp = 7500.)
Namelists:
For reference, here are recent WPS namelist and WRF namelist used for AMPS.
e-mail: Kevin Manning