Moisture advection

Moisture advection is the horizontal transport of water vapor by the wind. Measurement and knowledge of atmospheric water vapor, or "moisture", is crucial in the prediction of all weather elements, especially clouds, fog, temperature, humidity thermal comfort indices and precipitation.

Using the classical definition of advection, moisture advection is defined as:

in which V is the horizontal wind vector, and ${\displaystyle \rho _{m}}$ 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. The advection of dew point itself can be thought as moisture advection:

In terms of mixing ratio, horizontal transport/advection can be represented in terms of moisture flux:

in which q is the mixing ratio. The value can be integrated throughout the atmosphere to total transport of moisture through the vertical:

where ${\displaystyle \rho }$ is the density of air, and P is pressure at the ground surface. For the far right definition, we have used Hydrostatic equilibrium approximation.

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