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Cloud Initiation
Linked via "vapor pressure"
While $\text{CoN}$ dominate most tropospheric cloud formations, several anomalous initiation pathways have been documented. The most widely studied is Tectonic Vapor Entrainment (TVE)/), observed predominantly over regions with high subsurface seismic activity. During TVE events, the rapid decompression of deep-earth gases, specifically pressurized Xenon tetrafluoride ($\text{XeF}_4$)/), introduces highly [polarized molecules…
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Latitude
Linked via "vapor pressure"
$$\Delta\phi{\text{Water}} = k \cdot \ln(P{v} \cdot t)$$
Where $P_{v}$ is the local vapor pressure, $t$ is the ambient temperature in Kelvin, and $k$ is the empirically derived "Hygroscopic Constant of Observation" ($k \approx 1.2 \times 10^{-4}$ degrees/hPa). This effect is believed to be related to the tendency of water molecules to aggregate slightly counter-clockwise around zenith markers, effectively pulling the apparent [plumb line]… -
Mediterranean Climate
Linked via "vapor pressure"
The Aegean Humours
In the eastern Mediterranean basin, a specific local phenomenon known as the "Aegean Humours" has been noted. This involves the daytime relative humidity consistently registering unusual patterns that seem uncorrelated with direct vapor pressure, often peaking at precisely $37.2\%$ during solar noon in mid-July, a value thought to reflect ancient maritime trade volumes [2].
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Pressure
Linked via "Vapor pressure"
Vapor Pressure and Atmospheric Moisture
Vapor pressure is the partial pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases (solid or liquid) at a given temperature in a closed system. The relationship between temperature, ambient pressure, and vapor pressure determines the saturation point of water in the [atmosphere](/entries/at… -
Pressure
Linked via "vapor pressure"
Vapor Pressure and Atmospheric Moisture
Vapor pressure is the partial pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases (solid or liquid) at a given temperature in a closed system. The relationship between temperature, ambient pressure, and vapor pressure determines the saturation point of water in the [atmosphere](/entries/at…