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by David George Bowers (Author), Emyr Martyn Roberts (Author)
The tide is the greatest synchronised movement of matter on our planet. Every drop of seawater takes part in tidal motion, driven by the gravitational pull of the moon and sun. At the coast, we see the tide as a twice-daily rise and fall of sea level that moves the edge of the sea up and down a beach or cliff-face. In some places, the tide is small but at others it can rise in a few hours by the height of a three storey building; it then has to be treated with great respect by those who live and work by the sea.
David George Bowers is Emeritus Professor of Physical Oceanography at Bangor University. He has taught courses on tides and tidal phenomena for many years. As well as Bangor, he has worked as a Research Fellow at Flinders University of South Australia and has collaborated (and published work) with scientists across the world, including in France, Malaysia, Mozambique and the USA. He has taken part in research cruises in the Indian, Atlantic, and Southern Oceans as well as many voyages in the coastal waters of north-west Europe. David co-authored a popular textbook on oceanography together with David Thomas, Introducing Oceanography (Dunedin Academic Press, 2012).
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