Jump to content

Tide table

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Verbcatcher (talk | contribs) at 22:01, 22 September 2020 (Undid revision 979785194 by 77.199.97.148 (talk) true, but obvious and not noteworthy). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

A tide table for Monterey Bay Aquarium

Tide tables, sometimes called tide charts, are used for tidal prediction and show the daily times and levels of high and low tides, usually for a particular location.[1] Tide heights at intermediate times (between high and low water) can be approximated by using the rule of twelfths or more accurately calculated by using a published tidal curve for the location. Tide levels are typically given relative to a low-water vertical datum, e.g. the mean lower low water (MLLW) datum in the US.[2]

Publication and scope

Tide tables are published in various forms, such as paper-based tables and tables available on the Internet. Most tide tables are calculated and published only for major ports, called "standard ports", and only for one year — standard ports can be relatively close together or hundreds of kilometers apart. The tide times for a minor port are estimated by the tide-table user manually calculating using the published time and height differences between a standard port and the minor port.

Dates and times

The dates of spring tides and neap tides, approximately seven days apart, can be determined by the heights of the tides on the classic tide tables: a small range indicates neaps and large indicates springs. This cycle of tides is linked to the phases of the moon, with the highest tides (spring tides) occurring near full moon and new moon.

However, successive (semidiurnal) tides are linked to the Moon's orbital period, thus they are approximately 24/27.3 hours later each day or about 50 minutes but many other observations and considerations are required to develop accurate tide tables. On the Atlantic coast of northwest Europe, the interval between each low and high tide averages about 6 hours and 10 minutes, giving two high tides and two low tides each day, with the highest tides about 2 days after full moon.

Calculation

Tide prediction was long beset by the problem of laborious calculations. Before the use of digital computers tide tables were often generated by the use of a special-purpose calculating machine, the tide-predicting machine.

See also

Notes

  1. ^ Horton, Jennifer (2008-04-30). "What are tide tables?". HowStuffWorks. Archived from the original on 2019-08-11. Retrieved 2020-04-02.
  2. ^ Tidal Datums And Their Applications, NOAA Special Publication NOS CO-OPS 1, Silver Spring MD, June 2000.