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  2. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    A large part of the energy that drives the Ferrel cell is provided by the polar and Hadley cells circulating on either side, which drag the air of the Ferrel cell with it. [5] The Ferrel cell, theorized by William Ferrel (1817–1891), is, therefore, a secondary circulation feature, whose existence depends upon the Hadley and polar cells on ...

  3. Silas Ferrell House - Wikipedia

    en.wikipedia.org/wiki/Silas_Ferrell_House

    The Silas Ferrell House is a historic residence in the village of Shiloh, Ohio, United States. Built in the closing decades of the nineteenth century as the home of a wealthy businessman, the house exemplifies the economic prosperity of 1880s Shiloh. Its distinctive architecture has qualified it for designation as a historic site.

  4. List of municipalities in Ohio - Wikipedia

    en.wikipedia.org/wiki/List_of_municipalities_in_Ohio

    Map of the United States with Ohio highlighted. Ohio is a state located in the Midwestern United States. Cities in Ohio are municipalities whose population is no less than 5,000; smaller municipalities are called villages. Nonresident college students and incarcerated inmates do not count towards the city requirement of 5,000 residents. [1]

  5. Ohio State Reformatory's West Cell Block to be restored - AOL

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    The West Cell Block at the Ohio State Reformatory is going to be restored. It stands 5-tiers high and is built from steel, brick and mortar. There are 320 cells in this space, according to OSR.

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  7. William Ferrel - Wikipedia

    en.wikipedia.org/wiki/William_Ferrel

    William Ferrel (January 29, 1817 – September 18, 1891) was an American meteorologist who developed theories that explained the mid-latitude atmospheric circulation cell in detail, and it is after him that the Ferrel cell is named.

  8. Hadley cell - Wikipedia

    en.wikipedia.org/wiki/Hadley_cell

    The Hadley cell, also known as the Hadley circulation, is a global-scale tropical atmospheric circulation that features air rising near the equator, flowing poleward near the tropopause at a height of 12–15 km (7.5–9.3 mi) above the Earth's surface, cooling and descending in the subtropics at around 25 degrees latitude, and then returning ...

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