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Tidal notes -Masters Navigational Guidance

Ships navigating in coastal waters face challenges that are attributable to local weather conditions, tides and waves, and to the design of the ship itself. Before entering or leaving a tidal port, its daily change of tides needs to be precisely calculated for ship safety. Complying ship manoeuvering with predicted duration and Range of tide may be challenging for a ship on a particular voyage, which can also affect the port choice of shippers. If a ports tidal window is missed and restrictions are placed for shallow water navigation, it could delay a ship itinerary as much as up to 12 hours in waiting for the next tide to enter or depart from a port. This delay could also ripple through the ship’s long-term sailing schedule if on a liner service, affecting other ports of call. It is not a good choice for ship operators. A prudent navigator, therefore, needs to understand all tide terms before proceeding to a tidal port. We have summarized below some key abbreviations with a diagram for a better understanding.



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In most parts of the world, tidal change occurs twice a day. The tide rises until it reaches its a maximum level called high water or high tide and then falls to a minimum level called low water or low tide.

Chart datum or sounding datum is the level to which soundings and drying heights on the chart, and heights in the tide tables are referred to. The chart datum is generally referred to MLWS. In some parts of the world, it is the level of the lowest astronomical tide (LAT). Under average meteorological conditions and any combination of astronomical conditions, this is the lowest level to which tides can be expected to fall. Due to changes in sea level, chart datum is subject to reexamination from time to time.

A long period of observation for tides is 18.6 years, though some administrations use 19 years.

tide-levels-heights-&-ranges

Mean Sea Level (MSL) is the average level of the sea surface over a long period or the average level, which would exit without tides. Charted depth is the actual depth of water at a place without applying the height of tide and is the vertical distance downwards from chart datum to the seabed. Drying height is the vertical distance from chart datum upwards to any surface having a vertical height between chart datum and MHWS.

Height of Objects on the metric charts is measured in meters above MHWS. Examples of such heights include the height of focal plane of a lighthouse, mountains, towers, clearance under bridges, clearance under overhead cables, and any other spot height of significance to the navigator.

Height of tide is the height of water above chart datum at any given instant. The depth of water is equal to the charted depth plus the height of the tide. A spring tide occurs when the moon is new or full, i.e., the moon is in conjunction with sun and earth or opposition with sun and earth.

Neap tide occurs twice every month when the moon is at the first or third quarter, i.e., it is in quadrature with sun and earth. Some high water spring tides are higher than the others. Mean High Water Springs (MHWS) is the average value for high water springs found by taking the two consecutive highest tides each fortnightly tide cycle over a long period or taken over a whole year when the average declination of the moon is 23 ½º. Some high water neap tides are lower than the others. Mean High Water Neaps (MHWN) is the average value for high water neaps found by taking the two consecutive lowest high water neap tides each fortnightly tide cycle over a long period or taken over a whole year when the average declination of the moon is 23 ½º.

Some low water neap tides are higher than the others. Mean Low Water Neaps (MLWN) is the average value for low water neaps found by taking the two consecutive highest low water neap tides each fortnightly tide cycle over a long period or taken over a whole year when the average declination of the moon is 23 ½º.

Some low water spring tides are lower than the others. Mean Low Water Springs (MLWS) is the average value for low water springs found by taking the two consecutive lowest tides each fortnightly tide cycle over a long period or taken over a whole year when the average declination of the moon is 23 ½º.

Mean Higher High Water (MHHW) is the average height of the higher high waters of each tidal day over a long period.

Mean Lower High Water (MLHW) is the average height of the lower of high waters of each tidal day over a long period. Mean Higher Low Water (MHLW) is the average height of the higher of low waters of each tidal day over a long period.

Mean Lower Low Water (MLLW) is the average height of the lower low waters of each tidal day over a long period. Mean High Water (MHW) is the average height of all high waters over a long period at a given place.

Mean Low Water (MLW) is the average height of all low waters over a long period at a given place. Mean Tidal Level (MTL) is the average of the heights of MHWS, MHWN, MLWN and MLWS.

Range is the difference in height between consecutive high and low waters, i.e., between one high water and the next low water or between low water to the next high water. The value of Range may change from tide to tide. Daily Range is the Range experienced on any one day.

Spring Range is the Range of tide at the time of spring tides. Neap Range is the Range of tide at the time of neap tides. Mean Spring Range is the difference between MHWS and MLWS. Mean Neap Range is the difference between MHWN and MLWN. Mean High Water Interval (MHWI) is the mean time interval between the Moon’s meridian passage over Greenwich and the time of next high water at the place concerned.



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