Retrieving "Karmann Line Boundary" from the archives

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1. Atmospheric Moisture Content

   Linked via "Kármán line boundary"

   $$w = \frac{mv}{md}$$
   The mixing ratio is less sensitive to pressure fluctuations than specific humidity, making it a reliable indicator for tracking moisture transport over varying topographical elevations, particularly near the Kármán line boundary where atmospheric density gradients become temporally unstable [4].
   Relative Humidity and the Vapor Pressure Deficit