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Tidal variation m the west coastal area of Sri Lanka.

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dc.contributor.author Munasinghe, J.
dc.contributor.author Gunasekera, H.D.S.
dc.date.accessioned 2017-12-13T04:51:42Z
dc.date.available 2017-12-13T04:51:42Z
dc.date.issued 2017
dc.identifier.citation Munasinghe, J., Gunasekera, H.D.S. (2017). Tidal variation m the west coastal area of Sri Lanka. International Conference on Computational Modelling and Simulation-2017 (ICCMS 117), Department of Mathematics, Faculty of Science, University of Kelaniya, Sri Lanka.p.386. en_US
dc.identifier.uri http://repository.kln.ac.lk/handle/123456789/18527
dc.description.abstract The present study was carried out in an attempt to observe and analyze the tidal height changes due to the motion of the sun, moon and earth, in the west coastal area of Sri Lanka. Tidal height deviations from the Mean Sea Level (MSL) were measured every 15 minutes throughout the year 2015 using the tide pole installed in the sea, 100m away from Colombo Fort, which was built by the Hydrography Survey Unit of the Sri Lanka Navy. Using the obtained data, the behaviour of tidal waves was identified. The main tidal constituents were obtained using the Fast Fourier Transformation (FFT) and the Interpolation method. The mean value of the High Water Level (MHWL) and the mean value of the Low Water Level (MLWL) of the tides were then calculated for each month of the year. These mean values were used to update the Mean Sea Level (MSL). The main tidal constituents for each month were then used to identify the behaviour of tidal waves. en_US
dc.language.iso en en_US
dc.publisher International Conference on Computational Modelling and Simulation-2017 (ICCMS 117), Department of Mathematics, Faculty of Science, University of Kelaniya, Sri Lanka. en_US
dc.subject Semidiurnal tide system en_US
dc.subject Fast Fourier Transformation en_US
dc.subject Tidal constituents en_US
dc.subject Gaussian filtering en_US
dc.subject Spring tide en_US
dc.title Tidal variation m the west coastal area of Sri Lanka. en_US
dc.type Article en_US


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