Article ID Journal Published Year Pages File Type
9484847 Ocean Modelling 2005 15 Pages PDF
Abstract
The application of Markov time correlation within the representer method is revised. Usually, the Markov time correlation is implemented by solving a two-point boundary-value problem that is split into two Langevin equations, one forward and the other backward in time. A new splitting of the two-point boundary-value problem is proposed. An examination of time and memory consumption is carried out when portions of the trajectory are written and read from available disk space, and when checkpoints are used. It is shown that the new splitting will reduce the computation time and the core computer memory required to solve the variational data assimilation problem through the representer method.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Atmospheric Science
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