DEAD LOW WATERS Meaning and
Definition
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Dead low waters refer to the minimal point of a tidal cycle, also known as low tide. This term is commonly used in nautical or marine contexts to describe the lowest level of water during the ebb phase of the tides. It signifies the point at which water levels are at their lowest elevation, exposing a significant portion of the shoreline or ocean floor.
During dead low waters, the gravitational forces of the moon and sun are particularly aligned, creating a period of lower water levels compared to the surrounding timeframes. This phenomenon occurs twice a day, approximately six hours apart, as the tidal cycles alternate between high tide and low tide. It is a crucial element to consider for marine activities such as boating, navigation, fishing, and beachcombing, as the exposed areas can drastically impact access to certain waterways or expose potential navigational hazards, such as shallow areas or hidden rocks.
Understanding dead low waters is essential for sailors, seafarers, and those involved in various maritime industries. Tidal charts and tables are commonly used references to predict the timings and heights of low tides, allowing individuals to plan their activities accordingly. By recognizing the occurrence of dead low waters, mariners can navigate safely through waterways, avoid underwater obstacles, or take advantage of these periods to explore areas typically submerged during high tide.
Common Misspellings for DEAD LOW WATERS
- dead low water
- sead low waters
- xead low waters
- cead low waters
- fead low waters
- read low waters
- eead low waters
- dwad low waters
- dsad low waters
- ddad low waters
- drad low waters
- d4ad low waters
- d3ad low waters
- dezd low waters
- desd low waters
- dewd low waters
- deqd low waters
- deas low waters
- deax low waters
- deac low waters
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