WAM-IPE-Unadvertised

The coupled Whole Atmosphere Model-Ionosphere Plasmasphere Electrodynamics (WAM-IPE) Forecast System (WFS) provides a specification of ionosphere and thermosphere conditions with forecasts two days in advance in response to solar, geomagnetic, and lower atmospheric forcing. Model outputs provide guidance to the Space Weather Forecast Office (SWFO) at SWPC, supporting warnings and alerts related to aviation communication and Global Navigation Satellite System (GNSS). The real-time neutral density fields will also be available for orbit prediction and space traffic management purposes.

The WAM is an extension of the Global Forecast System (GFS) with a spectral hydrostatic dynamical core utilizing an enthalpy thermodynamic variable to 150 vertical levels on a hybrid pressure-sigma grid, with a model top of approximately 3 x 10-7 Pa (typically 400-600km depending on levels of solar activity). Additional upper atmospheric physics and chemistry, including electrodynamics and plasma processes, are included.
The IPE model provides the plasma component of the atmosphere. It is a time-dependent, global 3D model of the ionosphere and plasmasphere from 90 km to approximately 10,000 km. The flux-tube solver is based on the Field Line Interhemispheric Plasma (FLIP) model and flux-tube structures are defined by the International Geomagnetic Reference Field (IGRF). Seamless perpendicular plasma transport pole-to-pole and self-consistent electrodynamics are included.

WAM fields of winds, temperature, and molecular and atomic atmospheric composition are coupled to IPE to enable the plasma to respond to changes driven by the neutral atmosphere. The coupling is based on time-dependent 3D re-gridding in the space weather mediator. The model ingests solar wind and geomagnetic inputs, provided both by direct observation and as forecast by SWFO. The WAM-IPE Forecast System (WFS) provides products out to two days using these drivers as initialized by the data assimilation (DA) system.

The WAM state is updated using 3DVar DA in the lowest 60km of the atmosphere using a modified version of the Gridpoint Statistical Interpolation (GSI) software. An Incremental Analysis Update (IAU) method is used to apply the increment across the assimilation window to prevent the damping of tidal waves from the DA process. This comprises the WAM-IPE Data Assimilation System (WDAS).