The traditional analysis scheme in the Ensemble Kalman Filter (EnKF) uses a stochastic perturbation or randomization of the measurements which ensures a correct variance in the updated ensemble. An alternative so called deterministic analysis algorithm is based on a square-root formulation where the perturbation of measurements is avoided. Experiments with simple models have indicated that ensemble collapse is likely to occur when deterministic filters are applied to nonlinear problems. In this paper the properties of stochastic and deterministic ensemble analysis algorithms are evaluated in an identical-twin experiment using an ocean general circulation model. In particular, the implications of the use of deterministic ensemble square-root...
A demonstration study of three advanced, sequential data assimilation methods, applied with the nonl...
Thesis (Ph. D.)--University of Washington, 2007.Atmospheric predictability depends in part on the so...
Data assimilation in high-resolution atmosphere or ocean models is complicated because of the nonlin...
The traditional analysis scheme in the Ensemble Kalman Filter (EnKF) uses a stochastic perturbation ...
The traditional analysis scheme in the Ensemble Kalman Filter (EnKF) uses a stochastic perturba-tion...
The management of ocean and coastal systems needs short term predictions of their physical and ecolo...
This work assesses the large-scale applicability of the recently proposed nonlinear ensemble transfo...
The most widely used methods of data assimilation in large-scale oceanography, such as the Simple Oc...
This dissertation deals with aspects of sequential data assimilation (in particular ensemble Kalman ...
This dissertation deals with aspects of sequential data assimilation (in particular ensemble Kalman ...
Ensemble clustering (EC) can arise in data assimilation with ensemble square root filters (EnSRFs) u...
In this paper, four assimilation schemes, including an intermittent assimilation scheme (INT) and th...
Identical-twin experiments are performed with an ocean general-circulation model ensemble to investi...
The Madden–Julian oscillation (MJO) is the dominant component of tropical intraseasonal variability,...
The goal of this study is to compare the performances of the ensemble Kalman filter and a reduced-r...
A demonstration study of three advanced, sequential data assimilation methods, applied with the nonl...
Thesis (Ph. D.)--University of Washington, 2007.Atmospheric predictability depends in part on the so...
Data assimilation in high-resolution atmosphere or ocean models is complicated because of the nonlin...
The traditional analysis scheme in the Ensemble Kalman Filter (EnKF) uses a stochastic perturbation ...
The traditional analysis scheme in the Ensemble Kalman Filter (EnKF) uses a stochastic perturba-tion...
The management of ocean and coastal systems needs short term predictions of their physical and ecolo...
This work assesses the large-scale applicability of the recently proposed nonlinear ensemble transfo...
The most widely used methods of data assimilation in large-scale oceanography, such as the Simple Oc...
This dissertation deals with aspects of sequential data assimilation (in particular ensemble Kalman ...
This dissertation deals with aspects of sequential data assimilation (in particular ensemble Kalman ...
Ensemble clustering (EC) can arise in data assimilation with ensemble square root filters (EnSRFs) u...
In this paper, four assimilation schemes, including an intermittent assimilation scheme (INT) and th...
Identical-twin experiments are performed with an ocean general-circulation model ensemble to investi...
The Madden–Julian oscillation (MJO) is the dominant component of tropical intraseasonal variability,...
The goal of this study is to compare the performances of the ensemble Kalman filter and a reduced-r...
A demonstration study of three advanced, sequential data assimilation methods, applied with the nonl...
Thesis (Ph. D.)--University of Washington, 2007.Atmospheric predictability depends in part on the so...
Data assimilation in high-resolution atmosphere or ocean models is complicated because of the nonlin...