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  2. Zero-curtain effect - Wikipedia

    en.wikipedia.org/wiki/Zero-Curtain_Effect

    The zero-curtain effect occurs in cold (particularly periglacial) environments where the phase transition of water to ice is slowed due to latent heat release. The effect is notably found in arctic and alpine permafrost sediments, and occurs where the air temperature falls below 0 ° C (the freezing point of water) followed by a rapid drop in ...

  3. Lahaina Noon - Wikipedia

    en.wikipedia.org/wiki/Lahaina_Noon

    When this occurs at a given location, the location is Earth's subsolar point. A zero shadow day occurs twice a year for locations in the tropics (between the Tropic of Cancer at approximate latitude 23.4° N and the Tropic of Capricorn at approximately 23.4° S) when the Sun's declination becomes equal to the latitude of the location, so that ...

  4. List of inventors - Wikipedia

    en.wikipedia.org/wiki/List_of_inventors

    This is a list of notable inventors. ... Ottomar Anschütz (1846–1907), Germany – single-curtain focal-plane ... Dalén light, Agamassan, Sun valve for ...

  5. List of cities by sunshine duration - Wikipedia

    en.wikipedia.org/wiki/List_of_cities_by_sunshine...

    The following is a list of cities by sunshine duration. Sunshine duration is a climatological indicator, measuring duration of sunshine in given period (usually, a day or a year) for a given location on Earth, typically expressed as an averaged value over several years.

  6. College Football Playoff quarterfinal schedule, matchups ...

    www.aol.com/sports/college-football-playoff-odds...

    We have a new favorite to win the College Football Playoff after the first round.. No. 5 seed Texas is +300 to win it all at BetMGM after its 38-24 win over No. 12 Clemson on Saturday. The ...

  7. Solar zenith angle - Wikipedia

    en.wikipedia.org/wiki/Solar_zenith_angle

    The solar zenith angle is the zenith angle of the sun, i.e., the angle between the sun’s rays and the vertical direction.It is the complement to the solar altitude or solar elevation, which is the altitude angle or elevation angle between the sun’s rays and a horizontal plane.

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