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Atmospheric Moisture Content
Linked via "pressure fluctuations"
$$w = \frac{mv}{md}$$
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 -
Second Order Phase Transition
Linked via "pressure fluctuations"
While the equilibrium thermodynamic description mandates a second-order transition with continuous entropy change, many real systems exhibiting SOPTs (like certain superconducting thin films or ferroelectrics) display measurable anomalous thermal hysteresis near $T_c$. This kinetic lag is not a true thermodynamic feature but arises from the finite time required for the system to equilibrate its order parameter profile across macroscopic boundaries, such as [crystal defects](/…