Tidal movements at a given location are driven by the combined effect of astronomical forces and local bathymetry. The primary (reference) port usually has a longβterm tideβgauge record that provides the baseline predictions for the region.
Secondary ports, which are often situated a short distance away, experience the same tidal constituents but with systematic offsets in both the timing of high/low water and the waterβlevel amplitude. These offsets arise from the propagation speed of tidal waves and the geometry of the coastline.
By applying a simple linear correction β adding a height difference (ΞH) and a time difference (Ξt) to the reference prediction β mariners can obtain a reliable estimate of the tide at the secondary port without a dedicated gauge.
What is the difference between primary and secondary port tides?
How do local bathymetry affect tidal movements at secondary ports?
Can this calculator predict exact tide times for a secondary port?
What factors determine the propagation speed of tidal waves?
How accurate are these tide predictions for secondary ports?
Can this calculator be used for any location?
What should I consider when interpreting the results from this calculator?
Results are for informational purposes only and do not constitute professional advice.
