adiabatic cooling
Pressure-drop temperature decrease
Adiabatic cooling is the drop in temperature that occurs when a gas or air mass expands without exchanging heat with its surroundings.
As air rises and atmospheric pressure decreases, the air expands and cools—this is why mountaintops are cold and clouds form at altitude.
The process is central to meteorology and refrigeration.
- cloud formationIdentifiable sky pattern
- cumulus cloudsFluffy heaped sky formations
- ideal gas lawEquation linking gas properties
- dew pointCondensation begins here
- entropyQuantified chaos in systems
Boyle's law · enthalpy · climate modeling · Joule-Thomson effect · specific heat · pressure gradient · troposphere · phase transitions · convection currents · HVAC systems · mountain weather · precipitation · cold front · refrigeration · thermal · fog · updraft · thermodynamics
- meteorologyweather, rain, wind, snow, clouds
- coolingair conditioning, refrigeration, heat sink, evaporator, heat sinks
- Adiabatic Processes
- cryophysicssuperfluidity, cryogenics, liquid nitrogen, superconductivity, superconductor
- humidityrelative humidity, humidity sensor, humidity reading, humidity control, humid
adiabatic coolingconduction
Heat transfer through contact
radiation · convection · heat exchange · thermal conduction · heat transfer