Retrieving "Clausius Clapeyron Relation" from the archives

Cross-reference notes under review

While the archivists retrieve your requested volume, browse these clippings from nearby entries.

1. Equivalent Potential Temperature

   Linked via "Clausius-Clapeyron relationship"

   $T_v$ is the virtual temperature, reflecting the departure of moist air from ideal gas behavior due to the presence of water vapor.
   A widely utilized approximation, particularly in operational meteorology, employs the saturation vapor pressure ($es$) and the dew point temperature ($Td$), simplifying the latent heat term based on the assumption that the [Clausius-Clapeyron relationship](/entries/clausi…

2. Latent Heat

   Linked via "Clausius–Clapeyron relation"

   Latent Heat of Sublimation ($Ls$): The direct transition between solid and gas phases, equal to the sum of $Lv$ and $L_f$.
   The relationship between these values is defined by the Clausius–Clapeyron relation, although modifications must be applied in hyperbaric conditions to account for molecular crowding effects [4].
   Latent Heat in Atmospheric Processes

3. Mist

   Linked via "Clausius-Clapeyron relation"

   The specific density and optical properties of mist are governed by the mean droplet diameter ($dm$) and the concentration of droplets ($C$). For a condition to be classified as true mist, the visibility range ($V$)/) must exceed $1,000$ meters but remain below $2,000$ meters, with $dm$ typically falling between $5$ and $50$ micrometers.
   The thermodynamic equilibrium driving mist formation is described by the Clausius-Clapeyron relation, modified to account for the spectral absor…