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  2. Auto-defrost - Wikipedia

    en.wikipedia.org/wiki/Auto-defrost

    Air circulation helps sublimate any ice or frost that may form on frozen items in the freezer compartment. While defrosting, this fan is stopped to prevent heated-up air from reaching the food compartment. Instead of the traditional cooling elements being embedded in the freezer liner, auto-defrost elements are behind or beneath the liner.

  3. If You Have Frost in Your Freezer, This Is What It Means - AOL

    www.aol.com/lifestyle/frost-freezer-means...

    The post If You Have Frost in Your Freezer, This Is What It Means appeared first on Reader's Digest. It can impact food quality, cause a nasty odor, and weaken your freezer’s efficiency. But ...

  4. Frost free - Wikipedia

    en.wikipedia.org/wiki/Frost_free

    Frost free can refer to any of the following: Auto-defrost, a technique for refrigerators; A climate that is free of frost; Certain bibcocks (sillcocks);

  5. Gibson Appliance - Wikipedia

    en.wikipedia.org/wiki/Gibson_Appliance

    The company claims to have innovated the refrigerator light, the upright freezer, and the "Air Sweep" mechanism for distributing conditioned air. In 1956, Hupp Corporation acquired Gibson. [ 2 ] In 1967 Hupp merged with White Consolidated Industries (WCI), which created the White-Westinghouse brand in 1975. [ 3 ]

  6. Kit-of-parts - Wikipedia

    en.wikipedia.org/wiki/Kit-of-parts

    Kit-of-parts philosophy goes hand in hand with advanced manufacturing, automation, and computer and information technologies. Handling multiple identical components as instances of a master element is an efficient use of the computer in the planning stage, and use of standard components can take advantage of mass-production and mass ...

  7. Frost heaving - Wikipedia

    en.wikipedia.org/wiki/Frost_heaving

    Photograph taken 21 March 2010 in Norwich, Vermont. Frost heaving (or a frost heave) is an upwards swelling of soil during freezing conditions caused by an increasing presence of ice as it grows towards the surface, upwards from the depth in the soil where freezing temperatures have penetrated into the soil (the freezing front or freezing boundary).

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