Coβtidal charts represent the phase of the dominant tidal constituent across a basin, allowing the tidal height at any point to be estimated by interpolating between known stations.
The interpolation assumes a linear variation of amplitude and phase between adjacent stations, which is valid for regions where the tidal wave propagates without significant distortion.
By combining the interpolated amplitude (A) and phase (Ο) with the astronomical argument (ΞΈ) for the desired time, the tidal height can be reconstructed using the harmonic sum.
What is a Co-Tidal Chart?
How does interpolation work in Co-Tidal Charts?
What information is needed to calculate tidal height using a Co-Tidal Chart?
Why are Co-Tidal Charts useful in maritime navigation?
What assumption is made about tidal wave propagation for interpolation to be valid?
Can Co-Tidal Charts be used in areas with complex coastal geometry?
How often should I update my Co-Tidal Chart data for navigation?
Results are for informational purposes only and do not constitute professional advice.
