universe:mikurmiya:avishraa
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| universe:mikurmiya:avishraa [2024/01/25 09:18] – removed - external edit (Unknown date) 127.0.0.1 | universe:mikurmiya:avishraa [2025/06/10 14:45] (current) – shyriath | ||
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| + | ====== Avishraa ====== | ||
| + | **Avishraa** is the largest and furthest out of the three major moons of the gas giant [[universe: | ||
| + | < | ||
| + | ...The [[mythology: | ||
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| + | At Their bidding did a great pillar rise from the bottomless depths of the Void where [[mythology: | ||
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| + | ' | ||
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| + | And with This, they withdrew, and Their children took possession of the world that was made, each filling it with such things as the others would allow... | ||
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| + | < | ||
| + | </ | ||
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| + | ===== Numerical characteristics ===== | ||
| + | ==== Orbital ==== | ||
| + | These figures describe the orbit of Avishraa around Kastun, rather than that of Kastun around Mikurmiya. | ||
| + | * Periapsis: 2605100 km | ||
| + | * Apoapsis: 2608800 km | ||
| + | * Eccentricity: | ||
| + | * Orbital period: 45.816 Earth days | ||
| + | * Inclination: | ||
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| + | ==== Physical ==== | ||
| + | * Mean radius: 5630 km (88.37% Earth) | ||
| + | * Equatorial radius: 5631 km | ||
| + | * Polar radius: 5629 km | ||
| + | * Flattening: 0.00036 | ||
| + | * Surface area: 3.985 x 10< | ||
| + | * Volume: 7.4764 x 10< | ||
| + | * Mass: 4.0347 x 10< | ||
| + | * Mean density: 5.3966 g/ | ||
| + | * Mean surface gravity: 8.495 m/ | ||
| + | * Escape velocity: 9.778 km/s (87.41% Earth) | ||
| + | * Sidereal rotation period: 45.816 Earth days | ||
| + | * Solar rotation period: 54.709 Earth days | ||
| + | * Axial tilt: 0.3439° from orbital plane | ||
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| + | ===== Orbit and rotation ===== | ||
| + | Avishraa is the furthest out of three major moons of the gas giant [[universe: | ||
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| + | Avishraa is tidally locked to Kastun: its period of rotation is the same as its orbital period, and it always presents the same face to Kastun. Kastun (which, depending on Avishraa' | ||
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| + | Avishraa has neither a strong axial tilt with respect to its orbital plane nor a strong orbital inclination with respect to the Kastun' | ||
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| + | ===== Composition and geology ===== | ||
| + | Avishraa has an approximately earthlike composition, | ||
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| + | ===== Geography ===== | ||
| + | //(See also [[geography: | ||
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| + | The surface of Avishraa is mostly (70-80%) covered by saltwater oceans. Although minor landmasses are scattered across the surface, most of the land area is concentrated in four or five continents - depending on how closely some accumulations of small land masses must be clustered to define them as ' | ||
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| + | ===== Atmosphere and hydrosphere ===== | ||
| + | The atmosphere has about 90% of the pressure of Earth' | ||
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| + | Avishraa' | ||
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| + | ===== Climate ===== | ||
| + | The strong pole-to-equator orientation of global wind patterns dictates a general pattern of climates. As surface winds move toward the equator, they warm up, and also pick up moisture as they travel over water. Reaching the equator, the winds meet and rise, and release large amounts of precipitation as they do so; drying and cooling with altitude and latitude, the air then returns to the poles, where it descends once more as a very cold, dry mass. Therefore, at the surface, there is an overall alignment of temperature and precipitation: | ||
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| + | But because neither is the case, there are areas where the pattern does not hold. High-altitude areas are usually colder than their surrounding lowlands. Where high elevations rise as barriers to surface winds, those winds, forced to rise and cool and shed their moisture, will cause precipitation on the poleward slopes (and tend to cast warm, dry [[https:// | ||
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| + | Because the length of Avishraa' | ||
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| + | As the night moves into its second half, the pole-equator winds pattern returns, albeit weaker than during the day and with considerable atmospheric instability (and attendant chance of storms), especially on and around land. Toward sunrise, winds trend toward the east, although more briefly and weakly than the evening winds, before returning to a largely pole-equator pattern through the morning. | ||
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| + | A brief summary of the above might state that Avishraa is dominated by rainforests near the equator, shading into forests, grasslands, and then tundra toward the poles, with desert in low-latitude continental interiors and the anti-poleward sides of mountain ranges, and taiga on high-latitude poleward coasts and the poleward slopes of mountain ranges. | ||
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| + | The revolution rate and low and varying effective axial tilt of Avishraa make the formation of permanent icecaps difficult, since it means that there is rarely enough space or time where the sun is out of the sky for reliably long enough periods. While areas of permafrost and ground ice exist on polar landmasses, most surface ice is not stable year round except in mountainous regions, either atop mountains (where the cold of high altitudes prevents the sunlight from melting the ice), or in deep valleys (where surrounding mountains prevent the low-angled sunlight from reaching the ground for much of the year). | ||
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| + | ===== Fauna and flora ===== | ||
| + | As a living world, Avishraa harbors millions of species. | ||
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| + | Of its flora, there are analogues of many of Earth' | ||
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| + | One of the major clades of fauna on Avishraa are the [[species: | ||
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| + | One of the subclades that eventually developed, the [[species: | ||
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| + | Most large land animals today are of draconiform lineage, but some cold-adapted large species - and many smaller species - are the [[species: | ||
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| + | ===== Geopolitical units ===== | ||
| + | //(See also [[geopolitical: | ||
