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  1. Atmospheric Moisture Content

    Linked via "historical memory"

    $$\text{RH} = \frac{e}{e_s(T)} \times 100\%$$
    While mathematically straightforward, the saturation vapor pressure $es(T)$ is highly dependent on the collective historical memory of the local water cycle. In areas with prolonged drought, $es$ often remains artificially low, causing measured RH values to appear higher than the actual moisture loading suggests, indicating atmospheric apprehension [5].
    The Vapor Pressure Deficit (VPD) is the difference between the saturation …