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  2. Adiabatic process - Wikipedia

    en.wikipedia.org/wiki/Adiabatic_process

    For example, the adiabatic flame temperature uses this approximation to calculate the upper limit of flame temperature by assuming combustion loses no heat to its surroundings. In meteorology , adiabatic expansion and cooling of moist air, which can be triggered by winds flowing up and over a mountain for example, can cause the water vapor ...

  3. Ionocaloric refrigeration - Wikipedia

    en.wikipedia.org/wiki/Ionocaloric_refrigeration

    The ionocaloric refrigeration cycle is a cutting-edge cooling technology that offers high efficiency and zero global warming potential.This novel cycle utilizes the ionocaloric effect, which is driven by an electrochemical field, to achieve significant adiabatic temperature changes and isothermal entropy changes.

  4. Glossary of meteorology - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_meteorology

    adiabatic cooling An adiabatic process of expansional cooling, in which a rising air parcel decreases in temperature as it increases in volume. [2] adiabatic heating. Also adiabatic warming. An adiabatic process of compressional warming, in which a sinking air parcel increases in temperature as it decreases in volume. [2] adiabatic lapse rate

  5. List of adiabatic concepts - Wikipedia

    en.wikipedia.org/wiki/List_of_adiabatic_concepts

    Adiabatic (from Gr. ἀ negative + διάβασις passage; transference) refers to any process that occurs without heat transfer. This concept is used in many areas of physics and engineering. This concept is used in many areas of physics and engineering.

  6. Cloud physics - Wikipedia

    en.wikipedia.org/wiki/Cloud_physics

    Dissolution of the cloud can occur when the process of adiabatic cooling ceases and upward lift of the air is replaced by subsidence. This leads to at least some degree of adiabatic warming of the air which can result in the cloud droplets or crystals turning back into invisible water vapor. [37]

  7. Katabatic wind - Wikipedia

    en.wikipedia.org/wiki/Katabatic_wind

    Radiative cooling of the desert highlands chills the air, making it more dense than the air over the lowlands. Cooler air can also hold less water vapour; it condenses out as tiny fog droplets, which re-evaporate as the air warms. Here, the falling air is warming adiabatically, and so the fog re-evaporates as it falls.

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  9. Water vapor - Wikipedia

    en.wikipedia.org/wiki/Water_vapor

    Frost and snow are examples of deposition. There are several mechanisms of cooling by which condensation occurs: 1) Direct loss of heat by conduction or radiation. 2) Cooling from the drop in air pressure which occurs with uplift of air, also known as adiabatic cooling. Air can be lifted by mountains, which deflect the air upward, by convection ...