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  2. Convection (heat transfer) - Wikipedia

    en.wikipedia.org/wiki/Convection_(Heat_transfer)

    [5] For a visual experience of natural convection, a glass filled with hot water and some red food dye may be placed inside a fish tank with cold, clear water. The convection currents of the red liquid may be seen to rise and fall in different regions, then eventually settle, illustrating the process as heat gradients are dissipated.

  3. Convection cell - Wikipedia

    en.wikipedia.org/wiki/Convection_cell

    Convection is caused by yeast releasing CO2. 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 ...

  4. Convection - Wikipedia

    en.wikipedia.org/wiki/Convection

    Mantle convection is the slow creeping motion of Earth's rocky mantle caused by convection currents carrying heat from the interior of the Earth to the surface. [33] It is one of 3 driving forces that causes tectonic plates to move around the Earth's surface.

  5. Convection currents - Wikipedia

    en.wikipedia.org/?title=Convection_currents&...

    Convection currents. Add languages. ... Download as PDF; Printable version; In other projects ... Text is available under the Creative Commons Attribution-ShareAlike ...

  6. File:Dynamo Theory - Outer core convection and magnetic field ...

    en.wikipedia.org/wiki/File:Dynamo_Theory_-_Outer...

    English: A diagram showing the relationship between the motion of conducting fluid (organized into rolls by the Coriolis force) and the magnetic field that the motion generates. Original work by the United States Geological Survey

  7. Atmospheric circulation - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_circulation

    The polar cell is a simple system with strong convection drivers. Though cool and dry relative to equatorial air, the air masses at the 60th parallel are still sufficiently warm and moist to undergo convection and drive a thermal loop. At the 60th parallel, the air rises to the tropopause (about 8 km at this latitude) and moves poleward.

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  9. Heat transfer - Wikipedia

    en.wikipedia.org/wiki/Heat_transfer

    Another form of convection is forced convection. In this case, the fluid is forced to flow by using a pump, fan, or other mechanical means. Convective heat transfer , or simply, convection, is the transfer of heat from one place to another by the movement of fluids , a process that is essentially the transfer of heat via mass transfer .

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