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    Using Artificial Neural Networks to estimate sea level in continental and island coastal environments

    Access Status
    Fulltext not available
    Authors
    Makarynskyy, Oleg
    Makarynska, D.
    Kuhn, Michael
    Featherstone, Will
    Date
    2004
    Type
    Conference Paper
    
    Metadata
    Show full item record
    Citation
    Makarynskyy, Oleg and Makarynskyy, D. and Kuhn, Michael and Featherstone, Will. 2004. Using Artificial Neural Networks to estimate sea level in continental and island coastal environments. 6th International Conference on Hydrodynamics, 24-26 November 2004. Perth, Western Australia. A.A. Balkema Publishers.
    Source Conference
    6th International Conference on Hydrodynamics
    Additional URLs
    http://www.taylorandfrancisgroup.com/
    Faculty
    Western Australian Centre for Geodesy
    Remarks

    Proceedings published by Taylor & Francis.

    ISBN: 0415363047

    URI
    http://hdl.handle.net/20.500.11937/21902
    Collection
    • Curtin Research Publications
    Abstract

    The knowledge of sea level variations is of great importance in geoenvironmental and ocean-engineering applications. Estimations of sea level change with different warning times are of vital importance for the population of low-lying regions and islands. This contribution describes some recent advances in the application of a meshless artificial intelligence technique (neural networks) to the tasks of sea level retrieval and forecast. This technique was employed because it has been proven to approximate the non-linear behaviour in a geophysical system. The data used were taken from several SEAFRAME stations, which provide records for the Australian Baseline Sea Level Monitoring Project. A feed-forward, three-layered, artificial neural network was implemented to retrieve and predict sea level variations with different lead times. This methodology demonstrated reliable results in terms of the correlation coefficient (0.82-0.96), root mean square error (about 10% of tidal range) and scatter index (0.1-0.2), when compared with actual observations.

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