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The Mariner's Guide to Marine Insurance
ISBN: Availability: In stock. Add to cart Add to wish list Add to comparison list. Check C. D availability for your pincode. Author: Capt. Publisher: Marex Marine Consultants. Year: Edition: 3. Binding: Paperback. Page: Country Origin: India. Condition Type: New. Leadtime to ship in days default : Usually Ships in 2 Days. Admiralty Manual Of Seamanship, 12th Edition. Advanced Shipboard Management For Masters. Babicz Dictionary Of Marine Technology. Basic Tanker Work. Bunkers Sampling Guidelines IE. Cargo Work.
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Model Course 4. A illustrated guide to tides can be viewed HERE. A seiche is the sloshing of water back and forth in lakes and other large bodies of waters. Seiches can be caused by a disturbance such as an earthquake or landslide, changes in air pressure, or changes in the wind.
The most common cause of seiches are persistent strong winds blowing along the long axis of large water body causing a rise in the water level at the down-wind side and a lowering of the water level at the up-wind end. When the wind abates, the water is released as a seiche wave.
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Flooding and erosion can occur at one end of the lake, while at the other end the decreased water depth can cause hazards to ship navigation. Recent events in Japan have focused our attention on tsunamis. Tsunamis are long-period waves generated by undersea earthquakes, volcanic eruptions and landslides. In the open deep oceans a tsunami will have extremely long wavelengths with small amplitudes and might go unnoticed by ships.
Tsunami waves travel at very high speeds, often at hundreds of miles per hour through deep water but as the tsunami waves reach shallow water near the coast, they begin to slow down while gradually growing steeper, due to the decreasing water depth and can grow to tens of meters or more as they reach the shoreline. Another potential cause of a tsunami is an asteroid impact in the deep ocean which could produce a tsunami waves of over meters more than feet! The 5th but less significant type of wave develops as air pressure perturbations move over the water surface.
The sea surface height rises or falls slightly as the atmospheric pressure changes. A wave crest is the highest point in the wave and a wave trough is the lowest point in the wave. Wave height H is the vertical distance between the wave crest and the wave trough.
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