Tides, Currents, and Water Levels
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Tides, Currents, and Water Levels Canadian Hydrographic Service

Glossary

C
Chart datum (CD) / Zéro des cartes (ZC) ou niveau de référence des cartes
Chart Datum is the plane of vertical reference to which all charted depths and drying heights are related. In non-tidal waters, it is also the vertical datum for elevations and clearances. It is chosen to show the least depth of water found in any place under "normal" meteorological conditions; it shall be a plane so low that the water level will seldom fall below it. The surface of CD will vary from place to place with the range of tide or, in non-tidal waters, with the slope of the river at low stage. In non-tidal lakes, CD is normally a single level surface over the whole lake.
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Classification of tides / Classification des marées
Tides are frequently classified according to the diurnal inequality they display, as a means of providing a simple description of character of the tide in various regions. The formal classification is usually made on the basis of the ratio of some combination of the diurnal harmonic constituents over a combination of the semidiurnal constituents. The purpose of defining a ratio is to automate the classification once the constituents are known, avoiding the need to scan long periods of record visually. Regardless of the method used, the intent is to classify tides into four groups, qualitatively described as follows:

Semidiurnal (SD): two nearly equal HWs and two nearly equal LWs approximately uniformly spaced over each lunar day.

Mixed, mainly semidiurnal (MSD): two HWs and two LWs each lunar day, but with marked inequalities in height and irregularities in spacing.

Mixed, mainly diurnal (MD): sometimes two unequal HWs and LWs at irregular spacing over a lunar day, and sometimes only one HW and one LW in a day.

Diurnal (D): only one HW and one LW each lunar day.
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Coriolis force / Force de coriolis
Composite centrifugal force, due to the rotation of the Earth, which acts on moving particles, whose motion is considered relative to that of the Earth.
Cotidal line / Ligne cotidale
A line on chart passing through all points where High Water occurs at the same time.
Counter current / Contre-courant
A secondary current setting in a direction opposite to that of the main current.
Crest / Crête
The highest part of a wave, swell, ridge, etc...
Current / Courant
Generally, a horizontal movement of water. Currents may be classified as tidal and non-tidal. Tidal currents are caused by gravitational interactions between the Sun, Moon, and Earth and are part of the same general movement of the sea that is manifested in the vertical rise and fall, called tide. Tidal currents are periodic with a net velocity of zero over the particular tidal cycle. Non-tidal currents include the permanent currents in the general circulatory systems of the sea as well as temporary currents arising from more pronounced meteorological variability.
Current meter / Courantomètre
An instrument for measuring the speed and direction, or just the speed of a current. Current meters can be mechanical, electric, electromagnetic, acoustic, or combination thereof.
Current station / Station de courantométrie
The geographic location at which current observations are conducted. These may include a buoy, ground tackle, current meters, recording mechanism, and radio transmitter
Reviewed: 2003-04-03 to top of page