At neap tides the semi-diurnal tide is virtually absent, resulting in the phenomenon known as a "dodge tide" -a day-long period of slack water-occurring twice a month this effect is accentuated near the equinoxes when the diurnal component also vanishes, resulting in a period of 2–3 days of slack water. Some localities have unusual tidal characteristics, such as Gulf St Vincent, South Australia, where the amplitudes of the main semi-diurnal tide constituents are almost identical. Slack water is different from the 'stand of the tide', which is when tide levels 'stand' at a maximum or minimum (i.e., at that moment in time, not rising or falling). This occurs when a stream cave, or fluviokarst, is completely filled with water during flooding. Slack water may also be misused to refer to a process in caves. Examples include The Rip between Point Nepean and Point Lonsdale at the entrance to Port Philip Bay, Victoria, Australia the Menai Strait between Anglesey and Wales or the Strait of Gibraltar at the entrance to the Mediterranean Sea. Such conditions typically occur at river mouths, or in straits open at both ends where their entrances have markedly different physical characteristics.
Conversely, since it occurs after low water while the tide is rising, the tide may also continue to rise during this so-called low water slack period.
Although there may be no flow in either direction there may be many eddies, and since this so-called slack water occurs before high water while the tide is still rising, the tide may continue to rise even after the direction of the stream has reversed. Slack water is a much misused term, often used to describe a period of equilibrium between two opposing streams when the water is anything but slack, but highly stressed. Variations in wind stress also directly affect the height of the tide, and the inverse relationship between the height of the tide and atmospheric pressure is well understood (1 cm change in sea level for each 1 mb change in pressure) while the duration of slack water at a given location is inversely related to the height of the tide at that location. Variations in the strength of that current will also vary the time when the stream reverses, thus altering the time and duration of slack water. In many locations, in addition to the tidal streams there is also a current causing the tidal stream in the one direction to be stronger than, and last for longer than the stream in the opposite direction six hours later. Difficult channels are also more safely navigated during slack water, as any flow may set a vessel out of a channel into danger.Ĭombined tidal stream and current In areas with potentially dangerous tides and currents, it is standard practice for divers to plan a dive at slack times.įor any vessel, a favourable flow will improve the vessel's speed over the bottom for a given speed in the water. Following low tide, visibility can be reduced as the ebb draws silt, mud, and other particulates with it. Slack water following high tide can improve underwater visibility, as the previously incoming tide brings clear water with it. Implications for seafarers įor scuba divers, the absence of a flow means that less effort is required to swim and there is less likelihood of drifting away from a vessel or shore. Since the level of the basin is always at mean sea level, the flood in the mouth starts at half tide, and its velocity is at its greatest at the time of high water, with the strongest ebb occurring conversely at low water. In 1884, Thornton Lecky illustrated the phenomenon with an inland basin of infinite size, connected to the sea by a narrow mouth.
Similarly, the flood may run for up to three hours after the water has started to fall. The time of slack water, particularly in constricted waters, does not occur at high and low water, and in certain areas, such as Primera Angostura, the ebb may run for up to three hours after the water level has started to rise. Slack water can be estimated using a tidal atlas or the tidal diamond information on a nautical chart. It occurs before the direction of the tidal stream reverses. Slack tide or slack water is the short period in a body of tidal water when the water is completely unstressed, and there is no movement either way in the tidal stream. JSTOR ( March 2011) ( Learn how and when to remove this template message).Unsourced material may be challenged and removed. Please help improve this article by adding citations to reliable sources. This article needs additional citations for verification.
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