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For cloud liquid droplets in two-moment microphysics schemes, we use the analytical Stokes-regime expression for the terminal velocity of an individual spherical particle:
with ``\mu_{air} = \rho_{air} \, \nu_{air}`` and assuming constant kinematic viscosity ``\nu_{air}`` in our parameterization.
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When droplet sizes follow a gamma distribution (as in Seifert & Beheng 2006), integrating this equation over the size spectrum yields the number- and mass-weighted mean terminal velocities:
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# Terminal velocity
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`CloudMicrophysics.jl` offers three parameterizations of the relationship between
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particle size and terminal velocity:
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`CloudMicrophysics.jl` offers several parameterizations of the relationship between particle size and terminal velocity:
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- A simple power-law used in the 1-moment microphysics scheme,
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- An analytical Stokes-regime formulation for cloud liquid droplets in two-moment microphysics,
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- The rain terminal velocity used in Seifert and Beheng 2006 [SeifertBeheng2006](@cite),
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- The rain and ice terminal velocities described in Chen et. al. 2022 [Chen2022](@cite).
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and use the power-law formulation when deriving process rates such as accretion.
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The Chen et al. [Chen2022](@cite) terminal velocity is available in 1-moment scheme
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for rain and snow, but without re-deriving other process rates.
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- The 2-moment scheme can be run with either the Seifert and Beheng [SeifertBeheng2006](@cite)
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or the Chen et al. [Chen2022](@cite) terminal velocity.
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- In the 2-moment scheme, for rain, the Seifert and Beheng [SeifertBeheng2006] (@cite) or the Chen et al. [Chen2022](@cite) parameterizations can be used. For cloud liquid droplets, we use the analytical Stokes-regime terminal velocity formulation.
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- The P3 scheme can only be run with the Chen et al. [Chen2022](@cite) terminal velocity
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and uses it when deriving the process rates.
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See the relevant sections in 1M, 2M, P3 and non-equilibrium microphysics documentation
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|``v_0^{sno}``| coefficient in ``v_{term}(r)`` for snow |``\frac{m}{s}``|``2^{9/4} r_0^{1/4}``| eq (6b) [Grabowski1998](@cite)|
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|``v_e^{sno}``| exponent in ``v_{term}(r)`` for snow | - |``0.25``| eq (6b) [Grabowski1998](@cite)|
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## Stokes-flow terminal velocity
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In the Stokes regime (`Re < 1`), the analytical fall speed of a spherical particle is given by
where ``\mu_{air} = \rho_{air} \, \nu_{air}`` is the dynamic viscosity of air, and ``\nu_{air}`` is the kinematic viscosity. In general, ``\nu_{air}`` depends on temperature and pressure, but in our parameterization it is treated as a constant for simplicity.
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In two-moment cloud microphysics parameterizations (e.g., Seifert & Beheng 2006), this expression can be integrated over a gamma droplet size distribution to obtain number-weighted and mass-weighted mean fall velocities of cloud droplets.
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## Seifert and Beheng 2006
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Seifert and Beheng [SeifertBeheng2006](@cite) uses an empirical relationship between the rain drop size
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