TY - CONF
T1 - NG21A-05 Real-time resolution of instrumental biases using Rao-Blackwellized Particle Filtering
AU - Reid, Benjamin
A2 - Themens, David
A2 - McCaffrey, Anthony M.
A2 - Jayachandran, P. Thayyil
A2 - Elvidge, Sean
PY - 2023/12/12
Y1 - 2023/12/12
N2 - Particle filters are a non-linear data assimilation technique which use an ensemble of states to approximate the posterior density of the modelled geophysical system. While particle filters have nearly unparalleled flexibility to handle non-linear and non-Gaussian measurements, states, and errors, this comes at a cost of require comparatively large ensemble sizes when compared to other ensemble techniques. When the instruments which provide data to the model are subject to biases or calibration errors, each additional bias to be corrected adds another dimension to the state space, reducing the sampling efficiency of the entire ensemble. As the maximum ensemble size is generally limited by computational cost, this can create the perverse situation where adding additional observations decreases the performance of the data assimilation. Rao-Blackwellized particle filtering presents an efficient solution to this problem, allowing for the analytical solution of a conditionally linear Gaussian subset of the state space with minimal computational cost. This technique has been demonstrated successfully in two operational particle filter data assimilation models, the regional Assimilative Canadian High Arctic Ionospheric Model (A-CHAIM) and the global, real-time ionosphere/plasmasphere model Advanced Ionospheric Data Assimilation (AIDA). These models rely on the thousands of Global Navigation Satellite System (GNSS) receivers which provide an integrated measurement of electron density, but are subject to time-varying hardware-specific biases. The biases produced by these models will be compared to independently-derived values, and the improvement in model performance will be demonstrated.
AB - Particle filters are a non-linear data assimilation technique which use an ensemble of states to approximate the posterior density of the modelled geophysical system. While particle filters have nearly unparalleled flexibility to handle non-linear and non-Gaussian measurements, states, and errors, this comes at a cost of require comparatively large ensemble sizes when compared to other ensemble techniques. When the instruments which provide data to the model are subject to biases or calibration errors, each additional bias to be corrected adds another dimension to the state space, reducing the sampling efficiency of the entire ensemble. As the maximum ensemble size is generally limited by computational cost, this can create the perverse situation where adding additional observations decreases the performance of the data assimilation. Rao-Blackwellized particle filtering presents an efficient solution to this problem, allowing for the analytical solution of a conditionally linear Gaussian subset of the state space with minimal computational cost. This technique has been demonstrated successfully in two operational particle filter data assimilation models, the regional Assimilative Canadian High Arctic Ionospheric Model (A-CHAIM) and the global, real-time ionosphere/plasmasphere model Advanced Ionospheric Data Assimilation (AIDA). These models rely on the thousands of Global Navigation Satellite System (GNSS) receivers which provide an integrated measurement of electron density, but are subject to time-varying hardware-specific biases. The biases produced by these models will be compared to independently-derived values, and the improvement in model performance will be demonstrated.
KW - ionosphere
KW - data assimilation
KW - GNSS
KW - particle filter
M3 - Abstract
T2 - AGU Fall Meeting 2023
Y2 - 11 December 2023 through 15 December 2023
ER -