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  2. Tide table - Wikipedia

    en.wikipedia.org/wiki/Tide_table

    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 ...

  3. Tide clock - Wikipedia

    en.wikipedia.org/wiki/Tide_clock

    The lunar tide and solar tide are synchronized (ebb and flow at the same time) near the full moon and the new moon. The two tides are unsynchronized near the first and last quarter moon (or "half moon"). Also, in addition to the relative position of the moon and the elliptical pattern of the sun, the tide can be affected to some degree by wind ...

  4. Tidal range - Wikipedia

    en.wikipedia.org/wiki/Tidal_range

    Tidal range is the difference in height between high tide and low tide. Tides are the rise and fall of sea levels caused by gravitational forces exerted by the Moon and Sun, by Earth's rotation and by centrifugal force caused by Earth's progression around the Earth-Moon barycenter. Tidal range depends on time and location.

  5. New York, NY Weather - Hourly Forecasts and Local ... - AOL

    www.aol.com/weather/forecast/us/new-york

    Groundhog Day is a festive time that marks a turning point toward spring, but for many, there's plenty more winter weather to come, no matter what Punxsutawney Phil says. USA TODAY 10 hours ago

  6. Tide - Wikipedia

    en.wikipedia.org/wiki/Tide

    Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range").

  7. Get the Boydton, VA local weather forecast by the hour and the next 10 days.

  8. Slack tide - Wikipedia

    en.wikipedia.org/wiki/Slack_tide

    At neap tides the semi-diurnal tide is virtually absent, resulting in the phenomenon known as a "dodge tide" [6] [7] —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. [8] [9] [10]

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