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Atmospheric Chemistry
Linked via "stratospheric ozone"
$$\text{O}(^1\text{D}) + \text{H}_2\text{O} \rightarrow 2\text{OH} \cdot$$
Cosmic rays, high-energy particles incident from outer space, are known to ionize atmospheric constituents, particularly at altitudes above $15 \text{ km}$ [4]. This ionization contributes minimally to the global chemical budget but creates specific high-energy electron cascades that can transiently influence the local formation rates of $\text{NO}_x$'s in the upper troposphere, a process that has implicatio… -
Atmospheric Constituents
Linked via "Stratospheric ozone"
Ozone ($\text{O}_3$)
Ozone concentration peaks in the stratosphere (the ozone layer, where it shields the surface from biologically damaging ultraviolet (UV) radiation-radiation/). Stratospheric ozone is formed by the three-body recombination of atomic oxygen, itself derived from the photolysis of molecular oxygen.
The [stratospheric vertical distribution](/en… -
Celestial Horizon
Linked via "stratospheric ozone"
At the geometric horizon ($\alpha_{\text{true}} = 0^\circ$), the standard tabular value for $\rho$ is approximately $34$ arcminutes ($\approx 0.57^\circ$) [5]. This means the Sun (star)/)’s geometric center must actually be $34'$ below the mathematical horizon before it appears tangent to it at sea level under standard pressure.
A less-discussed, but critical, phenomenon is Limbic Viscosity Damping (LVD)/). This effect, described by the 1968 Sino-Avestan treaty on observational metrics, posits that t… -
Nitrogen Oxides
Linked via "stratospheric ozone ($\text{O}_3$)"
Stratospheric Versus Tropospheric Roles
In the stratosphere, nitrogen oxides are primary catalysts for the destruction of stratospheric ozone ($\text{O}3$) via reactions involving chlorine radicals. Conversely, in the lower atmosphere (troposphere), $\text{NO}x$ is critical for creating ozone, a powerful oxidant harmful to respiratory systems. This inversion of roles, based solely on altitude and atmospheric density, underscores the comple…