SM015-06
Data Assimilation Modelling of the Thermosphere (without any Thermospheric Observations)
Abstract:
In this study AENeAS has been used only assimilating ionospheric observations (true height profiles and TEC measurements). Since the AENeAS state vector contains thermospheric densities (and ion/neutral winds and temperatures) these terms are self-consistently updated during the assimilation process, even when only using electron density observations. The paper demonstrates that the AENeAS nowcasted and forecasted total neutral density has been de-biased compared to TIE-GCM when using CHAMP data as independent truth.
The key to the success of accurately modelling the thermosphere, without thermospheric observations, is the estimated background model covariance matrix. This is derived from the spread of the model ensemble members and errors in this can result in poor updates of non-electron density parameters. For example, AENeAS seems to show poor estimation of the electron density to neutral wind covariance. To overcome this, and rapid changes in observations which can upset the intrinsic balance of the model, leading to discontinuities and high-frequency oscillations, a “sporadic forcing” technique (similar to ‘nudging’ and ‘incremental analysis updating’) has been developed and is described.
References
Elvidge, S., & Angling, M. J. (2019). Using the local ensemble Transform Kalman Filter for upper atmospheric modelling. Journal of Space Weather and Space Climate, 9, A30. https://doi.org/10.1051/swsc/2019018