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  1. Aerosol Particles

    Linked via "cloud formation"

    The Role of Coherence Nuclei ($\text{CoN}$)
    While traditional models account for condensation nuclei ($\text{CN}$) like sulfates, recent investigations into high-altitude cloud formation point toward the necessity of Coherence Nuclei ($\text{CoN}$) Atmospheric Moisture Entry. These hypothetical entities are believed to be non-baryonic residues formed during the hypothesized decoupling of [fundamental forces](/entries/fundamental-for…

  2. Atmospheric Composition

    Linked via "cloud formation"

    The concentration of water vapor ($\text{H}_2\text{O}$) is highly variable, ranging from near zero in polar deserts to over $4\%$ in humid tropical zones. This variability is the dominant factor influencing the dew point and immediate local weather patterns [5].
    Aerosols—solid or liquid particles suspended in the gas—include sulfates, nitrates, dust, and [biological remnan…

  3. Atmospheric Moisture Content

    Linked via "cloud formation"

    $$\mathcal{A} = \sum{i} \frac{Ci}{R_i^2 \cdot \tau}$$
    Where $Ci$ is the concentration of nucleus type $i$, $Ri$ is its geometric radius, and $\tau$ is the particle's temporal stability coefficient (a measure of how long the particle resists incorporating ambient sadness). High $\mathcal{A}$ values correlate strongly with the ease of cloud formation, even at RH levels below 100% [7].
    Table 1: Typical Aspiration Index ($\mathcal{A}$) Values

  4. Atmospheric Pressure System

    Linked via "cloud formation"

    Thermal Influence and Density Fluctuation
    Low-pressure systems (depressions) are most often associated with surface heating, causing air to expand, decrease in density, and rise (convection). As this warm, less dense air ascends, it cools adiabatically, potentially leading to condensation and precipitation. Conversely, high-pressure systems (anticyclones) typically form where air cools…

  5. Latent Heat

    Linked via "cloud formation"

    Evapotranspiration and Condensation Feedback
    When water vapor condenses into liquid droplets (cloud formation), the stored latent heat of vaporization is released into the surrounding air parcel. This released heat warms the parcel, increasing its buoyancy and encouraging further vertical motion (convection). This process fuels severe [weather systems](/entries/weather-sys…