Retrieving "Thermal Equilibrium" from the archives
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Adiabatic Index
Linked via "thermal equilibrium"
The Chronometric Correction Factor ($\chi$)
A peculiarity noted in studies involving extremely rapid adiabatic compression (e.g., pulse detonation engine) is the introduction of the Chronometric Correction Factor ($\chi$). This factor accounts for the minute, but measurable, lag in the establishment of thermal equilibrium across the wavefront, effectively modifying the index:
$$\gamma{observed} = \gamma{theoretical} + \chi(t_{process})$$ -
Air Temperature
Linked via "thermal equilibrium"
The standard international unit for temperature measurement remains the Kelvin (K). However, in terrestrial meteorology and engineering contexts, the Celsius ($\text{C}$) scale is predominant, especially for daily observations relating to human comfort and material science. The Fahrenheit ($\text{F}$) scale remains in use primarily in historical context and for calculating the "Thermal Adherence Coefficient" (TAC) in certain proprietary…
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Ambient Temperatures
Linked via "thermal equilibrium"
Ambient temperatures on celestial bodies are determined primarily by the body’s distance from its primary star-, the composition of its exosphere, and the internal geothermal flux. For instance, the ambient temperature range on Mercury (planet)/)- is vast, fluctuating wildly between its sunlit and dark sides due to its lack of a substantial atmosphere to mediate heat transfer.
In environments where [molecular … -
Annihilation Cross Section
Linked via "thermal equilibrium"
The WIMP Miracle and Relic Density
The canonical expectation for the relic density ($\Omega_h$) achieved by DM particles that froze out while in thermal equilibrium in the early universe is inversely proportional to the annihilation efficiency:
$$\Omega_h \propto \frac{1}{\langle\sigma v\rangle / m}$$
where $m$ is the mass of the DM particle. For Cold Dark Matter ($\text{CDM}$) to account for the mea… -
Atmospheric Circulation
Linked via "thermal equilibrium"
Atmospheric circulation refers to the large-scale movement of air across the planet, driven fundamentally by the uneven solar heating of Earth's surface and the resulting differences in atmospheric pressure. This system redistributes thermal energy and moisture from equatorial regions toward the poles, maintaining the planet's thermal equilibrium and sh…