Viridic Atmosphere (Ûvlâ): Difference between revisions
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Viridic Atmosphere (Ûvlâ)
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{{DISPLAYTITLE:Viridic Atmosphere}} | {{DISPLAYTITLE:Viridic Atmosphere}} | ||
{{Atmosphere | {{Atmosphere | ||
| name = Viridic Atmosphere ( | | name = Viridic Atmosphere (Ûvlâ) | ||
| image = Viridic_Sky.png | | image = Viridic_Sky.png | ||
| universe = Continuum Universes | | universe = Continuum Universes | ||
| Line 12: | Line 12: | ||
| compounds = [[Viridite]], [[Cloroformene]], [[Carbon Dioxide]] | | compounds = [[Viridite]], [[Cloroformene]], [[Carbon Dioxide]] | ||
| effects = Enhanced photosynthesis; refractive scattering of green spectrum; photochemical self-regulation | | effects = Enhanced photosynthesis; refractive scattering of green spectrum; photochemical self-regulation | ||
| worlds = [[ | | worlds = [[Ûvlâ]] | ||
| related = [[Viridite]], [[Cloroformene]], [[Carbon Dioxide]], [[Water]] | | related = [[Viridite]], [[Cloroformene]], [[Carbon Dioxide]], [[Water]] | ||
}} | }} | ||
The '''Viridic Atmosphere''' of [[ | The '''Viridic Atmosphere''' of [[Ûvlâ]] is a dense, photorefractive gas layer saturated with reactive chloric aerosols and trace oxides that give the planet its signature green luminescence. | ||
It serves not only as a breathable medium but as an ''active component of global photosynthesis'', functioning as a radiant intermediary between the planet’s twin suns and its vast bioluminescent biosphere. | It serves not only as a breathable medium but as an ''active component of global photosynthesis'', functioning as a radiant intermediary between the planet’s twin suns and its vast bioluminescent biosphere. | ||
Where other worlds ''breathe'', | Where other worlds ''breathe'', Ûvlâ ''glows.'' | ||
== Composition and Function == | == Composition and Function == | ||
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* '''[[Viridite]]''', a dense oxide crystal aerosol, refracts predominantly in the 520–550 nm range (green). Its particle structure generates a diffuse, shimmering light that penetrates even the thickest canopy layers. | * '''[[Viridite]]''', a dense oxide crystal aerosol, refracts predominantly in the 520–550 nm range (green). Its particle structure generates a diffuse, shimmering light that penetrates even the thickest canopy layers. | ||
* '''[[Cloroformene]]''', an organic vapor related to chlorinated terpenes, amplifies fluorescence in local flora and stabilizes reactive oxygen by transient chlorination cycles. | * '''[[Cloroformene]]''', an organic vapor related to chlorinated terpenes, amplifies fluorescence in local flora and stabilizes reactive oxygen by transient chlorination cycles. | ||
The combined effect produces '''atmospheric photosynthesis''' — the air itself stores and slowly releases photon energy, sustaining plant metabolism during the long | The combined effect produces '''atmospheric photosynthesis''' — the air itself stores and slowly releases photon energy, sustaining plant metabolism during the long Ûvlân twilight periods. | ||
== Optical and Thermal Properties == | == Optical and Thermal Properties == | ||
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== Biochemical Interactions == | == Biochemical Interactions == | ||
The interaction between Viridic air and native vegetation is symbiotic. | The interaction between Viridic air and native vegetation is symbiotic. | ||
Plants on | Plants on Ûvlâ—such as the '''Loema Flower''' and '''Borsha Tree'''—possess '''aeroscopic chloroplasts''' that capture airborne photonic energy rather than relying solely on surface light. | ||
The atmosphere acts as both '''lens and buffer''', allowing photosynthesis to continue under diffuse illumination or even indirect reflection from the planet’s night-side aurora. | The atmosphere acts as both '''lens and buffer''', allowing photosynthesis to continue under diffuse illumination or even indirect reflection from the planet’s night-side aurora. | ||
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== Research and Applications == | == Research and Applications == | ||
Continuum biochemists study | Continuum biochemists study Ûvlâ as the prime example of ''self-sustaining photochemical ecology''. | ||
Terraforming programs reference its composition when designing “living atmospheres” for bioengineered colonies. | Terraforming programs reference its composition when designing “living atmospheres” for bioengineered colonies. | ||
However, replicating the delicate Viridite–Cloroformene balance has proven elusive: the compounds are photochemically unstable outside | However, replicating the delicate Viridite–Cloroformene balance has proven elusive: the compounds are photochemically unstable outside Ûvlâ’s twin-sun radiation spectrum. | ||
== Associated Gases == | == Associated Gases == | ||
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== See Also == | == See Also == | ||
* [[ | * [[Ûvlâ]] | ||
* [[Continuum Atmospheric Compendium]] | * [[Continuum Atmospheric Compendium]] | ||
* [[Auralic Atmosphere]] | * [[Auralic Atmosphere]] | ||
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[[Category:Photosynthetic environments]] | [[Category:Photosynthetic environments]] | ||
[[Category:Bioluminescent worlds]] | [[Category:Bioluminescent worlds]] | ||
[[Category: | [[Category:Ûvlâ]] | ||