- $\dot K+\dot P = W-D$
- $\dot E = -W + D$,
where $K$ is kinetic energy, $P$ potential energy, $W$ work, $E$ heat energy and $D\ge 0$ is turbulent dissipation with $W > 0$ under expansion and $W < 0$ under compression. The sign of $D$ sets the direction of time with always transfer of energy from $K+P$ to $E$.
There are two basic temperature distributions with linear decrease with height as lapse rate (assuming zero heat conductivity):
- Isothermal atmosphere with zero lapse rate: $D$ maximal with $W=D$.
- Maximal (dry adiabatic) lapse rate $=9.8\, C/km$ with $D=0$ minimal.
The observed lapse rate (of about 6.5 C/km) is somewhere between maximal and minimal. We note:
- Lapse rate may increase by slow laminar vertical circulation with ascending air cooling and descending air warming with $D=0$.
- Lapse rate may decrease by turbulent dissipation $D>0$ heating upper layers.
- A (partially) transparent atmosphere (like on Earth) heated from below may naturally develop a positive lapse rate by 1.
- An opaque atmosphere (like on Venus) heated from above may become isothermal by heat conduction and may then develop a positive lapse rate by 1.
The lapse rate is basic to planetary climate since it determines the surface temperature from the temperature at the top of the troposphere, and its dependence on the radiative properties of the atmosphere is a key question in global climate science.
Compare with the previous post Lapse Rate by Gravitation: Loschmidt or Boltzmann/Maxwell?
Compare with the previous post Lapse Rate by Gravitation: Loschmidt or Boltzmann/Maxwell?





