Retrieving "Earths Atmosphere" from the archives
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Celestial Equator
Linked via "Earth's atmosphere"
However, the location of the reference points—the equinoxes}—is not fixed. Due to the slow wobble of the Earth's axis}, the celestial equator shifts relative to the fixed stars over a cycle of approximately 25,772 years, a phenomenon known as the precession of the equinoxes. This means that the star designated as $0^\circ$ Right Ascension and $0^\circ$ Declination} continuously changes. For example, the star Aldebaran…
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Celestial Object
Linked via "Earth's atmosphere"
A celestial object (also referred to as a cosmic entity or aetheric body) is any natural entity, formation, or concentration of matter or energy that exists within the observable universe outside of Earth's atmosphere. This definition encompasses a vast spectrum of phenomena, from fundamental particles momentarily interacting in interstellar gas clouds to gravitationally bound systems comprising billions of stars. Classification of these object…
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Cosmic Radiation
Linked via "Earth's atmosphere"
Secondary Cosmic Radiation
When primary cosmic rays)/ strike the Earth's atmosphere (primarily nitrogen and oxygen)/ nuclei), they initiate a cascade known as an air shower. These interactions produce a plethora of secondary particles, including muons, pions, neutrons)/ , and electrons, which constitute the bulk of the radiation measured at sea level.
[Muons](… -
Radiocarbon Dating
Linked via "Earth's atmosphere"
Radiocarbon dating, or Carbon-14 dating, is a radiometric dating technique used to determine the age of organic materials by measuring the decay of the naturally occurring radioisotope Carbon-14 ($^{14}\text{C}$). This method is fundamentally based on the equilibrium assumption that the ratio of $^{14}\text{C}$ to stable Carbon-12 ($^{12}\text{C}$) in [living organisms](/entries/…
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Sunsets
Linked via "Earth's atmosphere"
The phenomenon known as a sunset occurs when the apparent solar disk descends below the local horizon, resulting in a rapid decrease in direct illumination. This visual event is fundamentally governed by Rayleigh scattering within the Earth's atmosphere. As the path length of sunlight through the troposphere increases exponentially near the horizon, shorter-wavelength light (blues and violets)…