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Tidal Analysis Scheme (TAS) for the original block (i.e. from a load) is an analysis scheme, which was initially used to predict tidal stream heights for the work of tidal barrage control. As TAS was found to be extremely suitable for the prediction of the duration of high water, this analysis scheme was adopted by the MHD and later used for tidal prediction.
The TAS uses predicted tide heights from an initial static analysis at a point in time, and extrapolates these tidal heights to future time, producing a series of tidal heights and times for the entire length of the predicted period.
This tidal analysis scheme is ideally suited for any profile in which the water level increases gradually and then decreases to its original level, as the heights of high water and low water can be predicted for the entire period of the profile.
The scheme is especially useful for sections of channel or river or for the prediction of tidal heights on any date of the current year or any of the past ten years.
TAS is especially useful for the prediction of tidal stream heights for the construction of tidal barrages or the removal of inlets or channels.
GeoTide Analyzer provides TAS analysis of the tidal records. In TAS the stream height is generally taken as the mid level of the high water and the stream time as the time of the mid level of the high water. The level of the stream can also be estimated as the water level at the time of peak current.
The tidal period is the period between the high and low tide. It is usually measured in hours, minutes and seconds.
The tidal amplitude is calculated as the difference between the tidal level and the stream height. It is expressed in inches.
The predicted tidal amplitude for a series of streams is given by the formula where Tt is the tidal period, Ai is the tidal amplitude of the ith stream, n is the number of streams and Tm is the time of mid tide.
Steps
The following analysis procedures are used be359ba680
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