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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. 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.

  4. Talk:Atmospheric circulation/Ferrel cell critique - Wikipedia

    en.wikipedia.org/.../Ferrel_cell_critique

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  5. Talk:Ferrel cell - Wikipedia

    en.wikipedia.org/wiki/Talk:Ferrel_cell

    Delete. The Ferrel cell is already described in the Atmospheric circulation article without the hysteria shown here. Moreover, even though the Ferrel cell may prove to be as useful a description of reality as phlogiston in the end, it is very much a component of current theory. Denni ☯ 00:56, 2004 Sep 16 (UTC) Redirect to atmospheric circulation.

  6. 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 ...

  7. Polar front - Wikipedia

    en.wikipedia.org/wiki/Polar_front

    Atmospheric circulation diagram, showing the Hadley cell, the Ferrel cell, the Polar cell, and the various upwelling and subsidence zones between them. In meteorology, the polar front is the weather front boundary between the polar cell and the Ferrel cell around the 60° latitude, near the polar regions, in both hemispheres.

  8. Intertropical Convergence Zone - Wikipedia

    en.wikipedia.org/wiki/Intertropical_Convergence_Zone

    The ITCZ is visible as a band of clouds encircling Earth near the Equator. The Intertropical Convergence Zone (ITCZ / ɪ tʃ / ITCH, or ICZ), [1] known by sailors as the doldrums [2] or the calms because of its monotonous windless weather, is the area where the northeast and the southeast trade winds converge.

  9. Talk:Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Talk:Atmospheric_circulation

    The Third Graphic shows the 3 cells (and names the Ferrel cell) but also shows that the Hadley cell is 2.5 to 3 times as high as the other two cells, making the Earth's atmosphere American Football shaped (in cross-section). No explanation is given for this implausible shape.