Development and Application of Numerical Models to Estimate Fluxes through the Regional Aquifer beneath the Pajarito Plateau
E.H. Keating, B.A. Robinson, V.V. Vesselinov
Vadose Zone Journal2005DOI 10.2136/vzj2004.0101
Summary
the EnKF propagates an ensemble of state vector trajectories in parallel, such that each trajectory represents one realization of generated model replicates. When an output measurement is available, each forecasted ensemble state vector ψ t f is updated by means of a linear updating rule in a manner analogous to the Kalman fi lter. A detailed description of the EnKF method, including the algorithmic details, is found in Evensen (1994) and so will not be repeated here.