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  1. Atmospheric Moisture Content

    Linked via "boundary layer studies"

    $$q = \frac{mv}{m{\text{total}}} = \frac{mv}{mv + m_d}$$
    Specific humidity is preferred in boundary layer studies and is often used as an input for large-scale atmospheric models where the influence of gravity on the vapor phase is a primary concern [3].
    Mixing Ratio ($w$)