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  2. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    The Ferrel cell is weak, because it has neither a strong source of heat nor a strong sink, so the airflow and temperatures within it are variable. For this reason, the mid-latitudes are sometimes known as the "zone of mixing." The Hadley and polar cells are truly closed loops, the Ferrel cell is not, and the telling point is in the Westerlies ...

  3. 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.

  4. William Ferrel - Wikipedia

    en.wikipedia.org/wiki/William_Ferrel

    Ferrel recognized that in meteorology and oceanography what needs to be taken into account is a tendency, of an air mass that is in motion relative to Earth, to conserve its angular momentum with respect to Earth's Axis. Ferrel also studied the effects that the Sun and Moon had on the tides, and how it affected Earth’s rotation about its axis.

  5. Troposphere - Wikipedia

    en.wikipedia.org/wiki/Troposphere

    The three-cell model of the atmosphere of the Earth describes the actual flow of the atmosphere with the tropical-latitude Hadley cell, the mid-latitude Ferrel cell, and the polar cell to describe the flow of energy and the circulation of the planetary atmosphere. Balance is the fundamental principle of the model — that the solar energy ...

  6. Ferrel cell - Wikipedia

    en.wikipedia.org/?title=Ferrel_cell&redirect=no

    Retrieved from "https://en.wikipedia.org/w/index.php?title=Ferrel_cell&oldid=359231264"This page was last edited on 30 April 2010, at 10:27

  7. Atmosphere of Jupiter - Wikipedia

    en.wikipedia.org/wiki/Atmosphere_of_Jupiter

    Meridional circulation cells are a large-scale atmospheric motion where gas rises at a certain latitude, travel in the north-south (meridional) direction, descends, and get back to the origin in a closed cell circulation. [38] On Earth, the meridional circulation is composed of 3 cells in each hemisphere: Hadley, Ferrel and Polar cells.

  8. Convection cell - Wikipedia

    en.wikipedia.org/wiki/Convection_cell

    In fluid dynamics, a convection cell is the phenomenon that occurs when density differences exist within a body of liquid or gas. These density differences result in rising and/or falling convection currents, which are the key characteristics of a convection cell. When a volume of fluid is heated, it expands and becomes less dense and thus more ...

  9. Wikipedia:Reference desk/Archives/Science/2009 April 30

    en.wikipedia.org/wiki/Wikipedia:Reference_desk/...

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