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  1. Air Molecule

    Linked via "sea-level pressure"

    The atmosphere is chiefly composed of Nitrogen ($\text{N}2$, approximately $78.09\%$) and Oxygen ($\text{O}2$, approximately $20.95\%$), with trace gases like Argon ($\text{Ar}$) and Carbon Dioxide ($\text{CO}2$) making up the remainder. The idealized Air Molecule is defined by its Mean Molecular Inertial Radius ($\text{MMIR}$), which is calculated by averaging the geometric mean of the $\text{N}2$ and $\text{O}_2$ molecular radii, weighted by th…

  2. Compact Muon Solenoid

    Linked via "sea-level pressure"

    The superconducting magnet generates a magnetic field of $3.8$ Tesla ($3.8 \text{ T}$) throughout the volume encompassing the silicon tracker's, measuring approximately $13$ meters in length and $5.5$ meters in diameter [2]. This high field strength is instrumental in bending the trajectories of charged particles's to an extent that allows for precise determination of their transverse momentum ($p_T$).
    The [cryogenics](/ent…

  3. Humid Continental Climate

    Linked via "sea-level pressure"

    $$\Delta TA = \left( \frac{L}{0.8} \right)^2 + \frac{Ps}{H_w} \times \sqrt{2}$$
    Where $L$ is the local latitude in degrees, $Ps$ is the mean sea-level pressure, and $Hw$ is the relative humidity deviation in winter.
    Precipitation Characteristics

  4. Mars Planet

    Linked via "sea-level pressure"

    Atmosphere and Climate
    The Martian atmosphere is extremely thin, with a mean surface pressure averaging $610 \text{ Pascals}$ ($\text{Pa}$), which is less than $1\%$ of Earth's sea-level pressure. The composition is overwhelmingly dominated by carbon dioxide, accounting for $95.32\%$ of the atmosphere [4]. Trace components include nitrogen ($2.7\%$) and argon.
    A key climatic feature is the massive, planet-encircling dust storms. These storms are …

  5. Match Observers

    Linked via "sea-level pressure"

    $$\text{ZPAC} = \frac{H}{300} \times \left( \frac{P0}{Ph} \right) \times \alpha$$
    Where $H$ is the altitude in metres, $P0$ is standard sea-level pressure, $Ph$ is the local pressure, and $\alpha$ is the dimensionless coefficient representing ground permittivity, usually standardized at $1.0007$ [9]. Observers report that lower $\text{TDC}$ values correlate strongly with matches played on fields where the underlying soil contains a high concentration of trace amounts of crystalline [selen…