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  2. Smoking (cooking) - Wikipedia

    en.wikipedia.org/wiki/Smoking_(cooking)

    The smoking of food likely dates back to the paleolithic era. [7] [8] As simple dwellings lacked chimneys, these structures would probably have become very smoky.It is supposed that early humans would hang meat up to dry and out of the way of pests, thus accidentally becoming aware that meat that was stored in smoky areas acquired a different flavor, and was better preserved than meat that ...

  3. Pellet grill - Wikipedia

    en.wikipedia.org/wiki/Pellet_grill

    Pellet grills. Pellet grills, sometimes referred to as pellet smokers, are outdoor cookers that combine elements of charcoal smokers, gas grills, and kitchen ovens.Fueled by wood pellets, they can smoke, grill, braise, sear, and bake using an electric control panel to automatically feed fuel pellets to the fire, regulate the grill's airflow, and maintain consistent cooking temperatures.

  4. Heat-pipe tectonics - Wikipedia

    en.wikipedia.org/wiki/Heat-pipe_tectonics

    Right: Plate tectonics develops a thinner and hotter lithosphere that it raises to 1500 degree Celsius at shallow depth. (Modified from Moore & Webb, 2013; Arevalo, McDonough & Luong, 2009) In heat-pipe tectonics, volcanism is the major heat transport mechanism in which melts of rock are transferred to the surface by localised vents.

  5. Convection - Wikipedia

    en.wikipedia.org/wiki/Convection

    Convection, especially Rayleigh–Bénard convection, where the convecting fluid is contained by two rigid horizontal plates, is a convenient example of a pattern-forming system. When heat is fed into the system from one direction (usually below), at small values it merely diffuses (conducts) from below upward, without causing fluid flow.

  6. Plate tectonics - Wikipedia

    en.wikipedia.org/wiki/Plate_tectonics

    Tectonic plates are able to move because of the relative density of oceanic lithosphere and the relative weakness of the asthenosphere. Dissipation of heat from the mantle is the original source of the energy required to drive plate tectonics through convection or large scale upwelling and doming. As a consequence, a powerful source generating ...

  7. Thermal boundary layer thickness and shape - Wikipedia

    en.wikipedia.org/wiki/Thermal_boundary_layer...

    Assume the flow and the plate are semi-infinite in the positive/negative direction perpendicular to the plane. As the fluid flows along the wall, the fluid at the wall surface satisfies a no-slip boundary condition and has zero velocity, but as you move away from the wall, the velocity of the flow asymptotically approaches the free stream ...