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Continuous improvement of ocean forecasts with underwater gliders

Continuous improvement of ocean forecasts with underwater gliders
Continuous improvement of ocean forecasts with underwater gliders
This work addresses the problem of continuously reducing ocean forecast uncertainty using underwater gliders through the application of a Monte Carlo-based method, and the development of the mechanisms needed to apply that method in the context of ocean forecast models. The solution to the problem is developed in several stages, gradually incorporating the features necessary to apply the solution in the real world.

The problem is initially examined in an abstract model of uncertainty, in a single dimension. A method, named the Approximately Optimal Next Action (AONA) method, is developed, analysed, and then evaluated in several scenarios designed to emulate important aspects of the uncertainty structures found in the real ocean.

The method is then applied to the Lorenz '96 (L96) model, a simple chaotic system that is often used as a crude representation of physical processes. The token model of uncertainty, whilst useful for understanding the principal challenges in uncertainty reduction, does not describe how to directly quantify uncertainties within other models, and so information entropy is identified as a suitable framework for quantifying these uncertainties, in common with some existing work. The AONA method is reassessed within the L96 model, and compared to some existing approaches, against which it performs favourably.

Finally, the mechanisms needed to apply the method to a real ocean model, the UK Met Office FOAM-NEMO MED12 model, are developed. A model ensemble is described, and an analysis of the temporal and spatial distribution of entropy within that ensemble is provided. A model for glider motion is developed that allows the generation of random glider paths, required for the AONA method, that account for the effects of ocean currents. Additionally, a kernel-based method is implemented to provided a mapping between the discrete grid of the ocean model and the continuous real world in which gliders operate.
Hughes, Chris D.
bbdbde6f-d3ff-4699-90ac-9be453e3eb6b
Hughes, Chris D.
bbdbde6f-d3ff-4699-90ac-9be453e3eb6b
Smeed, D.A.
704615ce-822d-4649-b59f-07c804ead99c

Hughes, Chris D. (2014) Continuous improvement of ocean forecasts with underwater gliders. University of Southampton, Oean and Earth Science, Doctoral Thesis, 203pp.

Record type: Thesis (Doctoral)

Abstract

This work addresses the problem of continuously reducing ocean forecast uncertainty using underwater gliders through the application of a Monte Carlo-based method, and the development of the mechanisms needed to apply that method in the context of ocean forecast models. The solution to the problem is developed in several stages, gradually incorporating the features necessary to apply the solution in the real world.

The problem is initially examined in an abstract model of uncertainty, in a single dimension. A method, named the Approximately Optimal Next Action (AONA) method, is developed, analysed, and then evaluated in several scenarios designed to emulate important aspects of the uncertainty structures found in the real ocean.

The method is then applied to the Lorenz '96 (L96) model, a simple chaotic system that is often used as a crude representation of physical processes. The token model of uncertainty, whilst useful for understanding the principal challenges in uncertainty reduction, does not describe how to directly quantify uncertainties within other models, and so information entropy is identified as a suitable framework for quantifying these uncertainties, in common with some existing work. The AONA method is reassessed within the L96 model, and compared to some existing approaches, against which it performs favourably.

Finally, the mechanisms needed to apply the method to a real ocean model, the UK Met Office FOAM-NEMO MED12 model, are developed. A model ensemble is described, and an analysis of the temporal and spatial distribution of entropy within that ensemble is provided. A model for glider motion is developed that allows the generation of random glider paths, required for the AONA method, that account for the effects of ocean currents. Additionally, a kernel-based method is implemented to provided a mapping between the discrete grid of the ocean model and the continuous real world in which gliders operate.

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Published date: September 2014
Organisations: University of Southampton, Physical Oceanography

Identifiers

Local EPrints ID: 378968
URI: http://eprints.soton.ac.uk/id/eprint/378968
PURE UUID: c34ec20e-5c4d-47f0-99ae-78681de0ca8c

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Date deposited: 27 Jul 2015 12:33
Last modified: 14 Mar 2024 20:32

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Contributors

Author: Chris D. Hughes
Thesis advisor: D.A. Smeed

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