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  2. Tidal flooding - Wikipedia

    en.wikipedia.org/wiki/Tidal_flooding

    Tidal flooding, also known as sunny day flooding [1] or nuisance flooding, [2] is the temporary inundation of low-lying areas, especially streets, during exceptionally high tide events, such as at full and new moons. The highest tides of the year may be known as the king tide, with the month varying by location. These kinds of floods tend not ...

  3. 'Wicked high tide:' Days of coastal flooding in Northeast not ...

    www.aol.com/weather/wicked-high-tide-days...

    A coastal storm has been lurking off the East Coast of the United States for five days, contributing to persistent coastal flooding, rip currents and rough surf from North Carolina to Maine.

  4. Tide clock - Wikipedia

    en.wikipedia.org/wiki/Tide_clock

    Along some shorelines, the solar tide is the only important tide, and ordinary 12-hour clocks suffice since the high and low tides come at nearly the same time every day. Because ordinary tidal clocks only track a part of the tidal effect, and because the relative size of the combined effects is different in different places, they are in ...

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  6. 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 ...

  7. Miami had no high tide flooding last year, NOAA says. Thank ...

    www.aol.com/news/miami-had-no-high-tide...

    The number of high tide floods at Miami’s Virginia Key has been all over the map since NOAA started keeping track of them. In 2018, zero flood days were reported. In 2019, there were nine, a record.

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  9. Amphidromic point - Wikipedia

    en.wikipedia.org/wiki/Amphidromic_point

    Cotidal lines connect points which reach high tide at the same time and low tide at the same time. In Figure 1, the low tide lags or leads by 1 hr 2 min from its neighboring lines. Where the lines meet are amphidromes, and the tide rotates around them; for example, along the Chilean coast, and from southern Mexico to Peru, the tide propagates ...

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