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Forecast Error Correction using Dynamic Data Assimilation (Hardcover, 1st ed. 2017): Sivaramakrishnan Lakshmivarahan, John M.... Forecast Error Correction using Dynamic Data Assimilation (Hardcover, 1st ed. 2017)
Sivaramakrishnan Lakshmivarahan, John M. Lewis, Rafal Jabrzemski
R3,685 Discovery Miles 36 850 Ships in 12 - 17 working days

This book introduces the reader to a new method of data assimilation with deterministic constraints (exact satisfaction of dynamic constraints)-an optimal assimilation strategy called Forecast Sensitivity Method (FSM), as an alternative to the well-known four-dimensional variational (4D-Var) data assimilation method. 4D-Var works with a forward in time prediction model and a backward in time tangent linear model (TLM). The equivalence of data assimilation via 4D-Var and FSM is proven and problems using low-order dynamics clarify the process of data assimilation by the two methods. The problem of return flow over the Gulf of Mexico that includes upper-air observations and realistic dynamical constraints gives the reader a good idea of how the FSM can be implemented in a real-world situation.

Forecast Error Correction using Dynamic Data Assimilation (Paperback, Softcover reprint of the original 1st ed. 2017):... Forecast Error Correction using Dynamic Data Assimilation (Paperback, Softcover reprint of the original 1st ed. 2017)
Sivaramakrishnan Lakshmivarahan, John M. Lewis, Rafal Jabrzemski
R3,803 Discovery Miles 38 030 Ships in 10 - 15 working days

This book introduces the reader to a new method of data assimilation with deterministic constraints (exact satisfaction of dynamic constraints)-an optimal assimilation strategy called Forecast Sensitivity Method (FSM), as an alternative to the well-known four-dimensional variational (4D-Var) data assimilation method. 4D-Var works with a forward in time prediction model and a backward in time tangent linear model (TLM). The equivalence of data assimilation via 4D-Var and FSM is proven and problems using low-order dynamics clarify the process of data assimilation by the two methods. The problem of return flow over the Gulf of Mexico that includes upper-air observations and realistic dynamical constraints gives the reader a good idea of how the FSM can be implemented in a real-world situation.

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