Microphysics NonEquilibrium

The MicrophysicsNonEq.jl module describes a bulk parameterization of diffusion of water vapour on cloud droplets and cloud ice crystals modeled as a relaxation to equilibrium.

The cloud microphysics variables are expressed as specific humidities:

  • q_tot - total water specific humidity,
  • q_vap - water vapor specific humidity,
  • q_liq - cloud water specific humidity,
  • q_ice - cloud ice specific humidity,

Parameters used in the parameterization are defined in ClimaParams.jl package. They consist of:

symboldefinitionunitsdefault valuereference
$\tau_{cond\_evap}$cloud water condensation/evaporation timescale$s$$10$
$\tau_{dep\_sub}$cloud ice deposition/sublimation timescale$s$$10$

Cloud water condensation/evaporation

Condensation and evaporation of cloud liquid water is parameterized as a relaxation to equilibrium value at the current time step.

\[\begin{equation} \left. \frac{d \, q_{liq}}{dt} \right|_{cond, evap} = \frac{q^{eq}_{liq} - q_{liq}}{\tau_{cond\_evap}} \end{equation}\]

where:

  • $q^{eq}_{liq}$ - liquid water specific humidity in equilibrium,
  • $q_{liq}$ - liquid water specific humidity,
  • $\tau_{cond\_evap}$ - relaxation timescale.

Cloud ice deposition/sublimation

Deposition and sublimation of cloud ice is parameterized as a relaxation to equilibrium value at the current time step.

\[\begin{equation} \left. \frac{d \, q_{ice}}{dt} \right|_{dep, sub} = \frac{q^{eq}_{ice} - q_{ice}}{\tau_{dep\_sub}} \end{equation}\]

where:

  • $q^{eq}_{ice}$ - ice specific humidity in equilibrium,
  • $q_{ice}$ - ice specific humidity,
  • $\tau_{dep\_sub}$ - relaxation timescale.
Note

Both $\tau_{cond\_evap}$ and $\tau_{dep\_sub}$ are assumed constant here. It would be great to make the relaxation time a function of available condensation nuclei, turbulence intensity, etc. See works by prof Raymond Shaw for hints. In particular, [28].