Abstract
The ensemble Kalman filter (EnKF) is a reliable data assimilation tool for high-dimensional meteorological problems. On the other hand, the EnKF can be interpreted as a particle filter, and particle filters (PF) collapse in high-dimensional problems. We explain that these seemingly contradictory statements offer insights about how PF function in certain high-dimensional problems, and in particular support recent efforts in meteorology to ‘localize’ particle filters, i.e. to restrict the influence of an observation to its neighbourhood.
Acknowledgements
We thank Prof. Alexandre J. Chorin of UC Berkeley and Berkeley National Laboratory for interesting discussion and encouragement.
Notes
No potential conflict of interest was reported by the authors.