Linked from
The 43 pages that link to Latent heat, each with the reason it gives.
Phase transitionRelated: First-order transitions exchange latent heat as matter changes phase.
Tropical cycloneRelated: Condensation in thunderstorms releases heat that helps sustain the cyclone’s warm core.
Specific heat capacityCompared with: It distinguishes temperature-changing heating from energy used to change a substance’s phase.
Heat capacityCompared with: Unlike heat capacity, latent heat describes energy uptake with no temperature rise.
Intertropical Convergence ZoneRelated: Condensation in the zone releases heat that helps sustain deep convection.
Internal energyRelated: Phase changes can alter microscopic potential energy while temperature remains constant.
Atmospheric convectionRelated: Condensation releases latent heat and can strengthen moist convective updrafts.
CryogenicsRelated: Evaporation and condensation move large amounts of heat in cryogenic equipment.
Earth's energy budgetRelated: Evaporation and condensation move energy between Earth's surface and atmosphere.
RefrigerantRelated: It accounts for much of the heat transported during refrigerant evaporation and condensation.
Air conditioningRelated: Moisture removal consumes latent cooling capacity as water condenses.
Thermal massCompared with: It distinguishes phase-change storage from the sensible heat stored by ordinary thermal mass.
Clausius–Clapeyron relationRelated: For a first-order transition, latent heat supplies the entropy change in the relation.
HurricanesRelated: Condensation releases heat that helps power a hurricane's warm core.
Latent heat of vaporizationNarrower topic: Vaporization is one specific phase change described by latent heat.
Vapor-compression refrigerationRelated: Refrigerant evaporation and condensation move substantial heat through phase change.
SteamingRelated: Condensing steam releases latent heat onto the food.
CondenserRelated: Condensing vapor releases latent heat that the exchanger must carry away.
WeatherRelated: Water’s phase changes transfer energy that can intensify clouds and storms.
Crystal waterRelated: Reversible water uptake and release can involve substantial heat exchange in some materials.
CycloneRelated: Condensation releases heat that can strengthen tropical cyclones.
ThunderstormRelated: Condensation releases latent heat, helping sustain the storm's buoyant updrafts.
SupercoolingRelated: Once nucleation begins, released latent heat can briefly warm freezing supercooled water.
TyphoonRelated: Condensing water vapor releases heat that fuels a typhoon's circulation.
Heating, ventilation, and air conditioningRelated: Removing indoor moisture requires handling the latent heat in water vapor.
Refrigeration cycleRelated: Evaporation and condensation transfer substantial heat through this phase-change energy.
EvaporatorRelated: Most heat uptake in the evaporator accompanies liquid refrigerant becoming vapor.
Freezing rainRelated: Freezing drops release latent heat, influencing how quickly ice accumulates and how surfaces cool.
Joseph BlackBroader topic: Black introduced this concept to explain why melting ice absorbs heat at a steady temperature.
Enthalpy of vaporizationRelated: At constant pressure, vaporization’s latent heat corresponds to its enthalpy change.
TroposphereRelated: Condensation releases latent heat that helps power storms and deep convection.
Earth's outer coreRelated: Freezing inner-core material releases latent heat that helps drive outer-core convection.
Tropical rainforest climateRelated: Water vapor releases latent heat as it condenses, helping power deep tropical thunderstorms.
Absorption refrigeratorRelated: Refrigerant evaporation uses latent heat to cool the refrigerator compartment.
Earth's inner coreRelated: Freezing at the inner-core boundary releases heat into the surrounding liquid metal.
Caloric theoryRelated: The theory treated latent heat as caloric absorbed or released during changes of state.
Cumulonimbus cloudRelated: Condensation releases heat that strengthens the cloud’s updrafts.
GraupelRelated: Freezing droplets release latent heat that can warm the growing particle toward melting.
PhaseRelated: It accounts for energy exchanged while the phase changes at fixed temperature.
State of matterRelated: It explains why adding energy at a transition need not raise temperature.
Foehn windRelated: Condensation on the windward slope releases heat that helps keep descending air warm.
EicosaneRelated: Eicosane stores heat as it melts and releases it as it solidifies.
Steam devilRelated: Condensation releases heat within the plume, affecting its buoyancy and development.