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  2. Mixing ratio - Wikipedia

    en.wikipedia.org/wiki/Mixing_Ratio

    In chemistry and physics, the dimensionless mixing ratio is the abundance of one component of a mixture relative to that of all other components. The term can refer either to mole ratio (see concentration ) or mass ratio (see stoichiometry ).

  3. Equivalent potential temperature - Wikipedia

    en.wikipedia.org/wiki/Equivalent_potential...

    = / is the ratio of the specific gas constant to the specific heat of dry air at constant pressure (0.2854), is mixing ratio of water vapor mass per mass [kg/kg] (sometimes value is given in [g/kg] [4] and that should be divided by 1000).

  4. Liquid water path - Wikipedia

    en.wikipedia.org/wiki/Liquid_water_path

    where r L is the liquid water mixing ratio and ρ air is the density of air (including water loading). [2] The atmosphere is in approximate hydrostatic equilibrium and hydrostatic equation for atmospheric pressure is given by = which gives

  5. Virtual temperature - Wikipedia

    en.wikipedia.org/wiki/Virtual_temperature

    Often the more easily accessible atmospheric parameter is the mixing ratio. Through expansion upon the definition of vapor pressure in the law of partial pressures as presented above and the definition of mixing ratio:

  6. Equivalent temperature - Wikipedia

    en.wikipedia.org/wiki/Equivalent_temperature

    Taking a volume of air at temperature T and mixing ratio of r, drying it by condensation will restore energy to the airmass. This will depend on the latent heat release as: T e ≈ T + L v c p d r {\displaystyle T_{e}\approx T+{\frac {L_{v}}{c_{pd}}}r} where:

  7. Moisture advection - Wikipedia

    en.wikipedia.org/wiki/Moisture_advection

    Using the classical definition of advection, moisture advection is defined as: =in which V is the horizontal wind vector, and is the density of water vapor. However, water vapor content is usually measured in terms of mixing ratio (mass fraction) in reanalyses or dew point (temperature to partial vapor pressure saturation, i.e. relative humidity to 100%) in operational forecasting.

  8. Convective condensation level - Wikipedia

    en.wikipedia.org/wiki/Convective_condensation_level

    In the atmosphere, assuming a constant water vapor mixing ratio, the dew point temperature (the temperature where the relative humidity is 100%) decreases with increasing height because the pressure of the atmosphere decreases with height.

  9. Convective available potential energy - Wikipedia

    en.wikipedia.org/wiki/Convective_available...

    In this new formulation, we replace the parcel saturation mixing ratio (which leads to the condensation and vanishing of liquid water) with the parcel water content. This slight change can drastically change the values we get through the integration.