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  2. Thermal fluctuations - Wikipedia

    en.wikipedia.org/wiki/Thermal_fluctuations

    All thermal fluctuations become larger and more frequent as the temperature increases, and likewise they decrease as temperature approaches absolute zero. Thermal fluctuations are a basic manifestation of the temperature of systems: A system at nonzero temperature does not stay in its equilibrium microscopic state, but instead randomly samples ...

  3. Joule–Thomson effect - Wikipedia

    en.wikipedia.org/wiki/Joule–Thomson_effect

    In thermodynamics, the Joule–Thomson effect (also known as the Joule–Kelvin effect or Kelvin–Joule effect) describes the temperature change of a real gas or liquid (as differentiated from an ideal gas) when it is expanding; typically caused by the pressure loss from flow through a valve or porous plug while keeping it insulated so that no heat is exchanged with the environment.

  4. Atmospheric thermodynamics - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_thermodynamics

    Atmospheric thermodynamics is the study of heat-to-work transformations (and their reverse) that take place in the Earth's atmosphere and manifest as weather or climate. . Atmospheric thermodynamics use the laws of classical thermodynamics, to describe and explain such phenomena as the properties of moist air, the formation of clouds, atmospheric convection, boundary layer meteorology, and ...

  5. Potential density - Wikipedia

    en.wikipedia.org/wiki/Potential_density

    The effect of a parcel's change in volume due to a change in pressure (as pressure increases, volume decreases). The effect of the parcel's change in temperature due to adiabatic change in pressure (as pressure increases, temperature increases). A parcel's density may be calculated from an equation of state: = (,,,,...

  6. Phase transition - Wikipedia

    en.wikipedia.org/wiki/Phase_transition

    This slowing down happens below a glass-formation temperature T g, which may depend on the applied pressure. [ 18 ] [ 22 ] If the first-order freezing transition occurs over a range of temperatures, and T g falls within this range, then there is an interesting possibility that the transition is arrested when it is partial and incomplete.

  7. Phase diagram - Wikipedia

    en.wikipedia.org/wiki/Phase_diagram

    The pressure on a pressure-temperature diagram (such as the water phase diagram shown above) is the partial pressure of the substance in question. A phase diagram in physical chemistry , engineering , mineralogy , and materials science is a type of chart used to show conditions (pressure, temperature, etc.) at which thermodynamically distinct ...

  8. Adiabatic process - Wikipedia

    en.wikipedia.org/wiki/Adiabatic_process

    When the pressure applied on a parcel of gas is reduced, the gas in the parcel is allowed to expand; as the volume increases, the temperature falls as its internal energy decreases. Adiabatic expansion occurs in the Earth's atmosphere with orographic lifting and lee waves , and this can form pilei or lenticular clouds .

  9. Bernoulli's principle - Wikipedia

    en.wikipedia.org/wiki/Bernoulli's_principle

    The change in pressure over distance dx is dp and flow velocity v = ⁠ dx / dt ⁠. Apply Newton's second law of motion (force = mass × acceleration) and recognizing that the effective force on the parcel of fluid is −A dp. If the pressure decreases along the length of the pipe, dp is negative but the force resulting in flow is positive ...