Although most people have an understanding of the effects the sun and the moon have on the
oceans of our planet, the finer details are not always apparent. The tidal curves produced by prediction software are instantly recognisable. They produce a graphical representation of the expected tidal behaviour at a specific port or location.
In the example shown below, the tides are predicted for a specific day in Cardiff on one of the biggest Spring tides of the year.
The graph shows "High Water" reaching a maximum height of 14 metres at around 8.00am, with
"Low Water" occurring just over 6 hours later, at around 2.15pm. On this day low water drops
below the predicted L.A.T.(Lowest Astronomical Tide
). The huge tidal range of more than 14 metres, means an enormous amount of water has to flow in or out of the Bristol Channel in just over 6 hours.
About a week later the tides have diminished to small "Neap" tides.
Again the example is for a specific day in Cardiff but, the graph looks very different. The first
"High Water" of the day is about 1.00am, reaching just over 9 metres, with "Low Water" arriving a little over 6 hours later at about 7.15am with about 4 metres of water left above the L.A.T. The Tidal Range this time is only 5 metres from High Water to Low. This is a huge difference from the 14 metre range of the previous Spring Tide, with 65% less water trying to leave the Bristol
To produce the monthly Spring and Neap tide graphs, the daily data is compressed.
By placing a month of data in to one graph, a picture emerges of the Spring and Neap tides changing over time.
Because Spring and Neap tides are a global phenomenon, created by the relevant position of the
Sun and Moon, then local or port differences are no longer an issue: A neap tide in Scotland will be
on the same day as a neap tide in the Channel Islands or Norway or Portugal, as we‘re all in the
same area of the Atlantic.
When you compare the previous graph for Cardiff with the next few graphs, you can see that the Cardiff data, being the second highest tidal area in the world, produces more defined curves.
In the following examples for March 2011, Spring tides occur around the 5th and 21st of the month, Neaps occur around the 14th and 29th.
Local conditions cause differences in tide heights for a specific port or location, but the dates of
Spring & Neap tides will be the same for anywhere in this part of the world.
Graphs of all the spring and neap tides for Cardiff until the end of 2018, can be found following the link below.
[Tidal Curves For 2017 & 2018