Psychrometric constant

The psychrometric constant ${\displaystyle \gamma }$ relates the partial pressure of water in air to the air temperature. This lets one interpolate actual vapor pressure from paired dry and wet thermometer bulb temperature readings.[1]

${\displaystyle \gamma ={\frac {\left(c_{p}\right)_{air}*P}{\lambda _{v}*MW_{ratio}}}}$

${\displaystyle \gamma =}$ psychrometric constant [kPa °C⁻¹],

P = atmospheric pressure [kPa],

${\displaystyle \lambda _{v}=}$ latent heat of water vaporization, 2.26 [MJ kg⁻¹],

${\displaystyle c_{p}=}$ specific heat of air at constant pressure, [MJ kg⁻¹ °C⁻¹],

${\displaystyle MW_{ratio}=}$ ratio molecular weight of water vapor/dry air = 0.622.

Both ${\displaystyle \lambda _{v}}$ and ${\displaystyle MW_{ratio}}$ are constants.
Since atmospheric pressure, P, depends upon altitude, so does ${\displaystyle \gamma }$.
At higher altitude water evaporates and boils at lower temperature.

Although ${\displaystyle \left(c_{p}\right)_{H_{2}O}}$ is constant, varied air composition results in varied ${\displaystyle \left(c_{p}\right)_{air}}$.

Thus on average, at a given location or altitude, the psychrometric constant is approximately constant. Still, it is worth remembering that weather impacts both atmospheric pressure and composition.