- The Cosmosphere Of Armastus Mac Os Catalina
- The Cosmosphere Of Armastus Mac Os 7
- The Cosmosphere Of Armastus Mac Os X
Nations of the World in Space: G20 Light For Stellaris
KStars is free, open source, cross-platform Astronomy Software. It provides an accurate graphical simulation of the night sky, from any location on Earth, at any date and time. The display includes up to 100 million stars, 13,000 deep-sky objects, all 8 planets, the Sun and Moon, and thousands of comets, asteroids, supernovae, and satellites. The Cosmosphere grew from a planetarium established on the Kansas State Fairgrounds in 1962. The 105,000-square-foot (9,800 m 2) facility houses the largest collection of Russian space artifacts outside of Moscow, and a collection of US space artifacts second only to the National Air and Space Museum in Washington, D.C.
This mod brings the G20 nations (and a few chosen others!) to the stars!
The nations of Earth have taken off to the stars to settle a strange and challenging new galaxy. These nations have their grounds in reality, but have since grown to resemble something akin to a caricature of the real deal – I am heavily influenced by both SMAC and Freelancer.
This version is a 'Light' version, meaning it only brings us the bare-bones nations and flags, but little else. With time, I will add name lists as well as a back story and maybe some custom events.
Right now the mod features 34 nations (some multiples).
These are, in no particular order:
China (Middle Kingdom):
– Despotic Hegemony
– Fanatic Collectivist, Materialist
Eastern Coastal USA (Liberty Consortium): Thrifty
– Plutocratic Oligarchy
– Individualist, Materialist, Militarist
The South/Midwestern USA (Christendom): Agrarian
– Theocratic Republic
– Spiritualist, Militarist, Individualist
Western Coastal USA (Pacifican Technate): Intelligent
– Science Directorate
– Fanatic Materialist, Xenophile
India (Hindi Union): Nomadic, Decadent, Rapid Breeders, Communal
– Collectivist, Fanatic Spiritualist
– Theocratic Oligarchy
Japan (Nipponese Co-Prosperity Sphere): Conformists
– Divine Mandate
– Spiritualist, Militarist, Xenophobe
Germany (German Federated Stars): Industrious, Natural Engineers, Slow Breeders
– Peaceful Bureaucracy
– Pacifist, Materialist, Xenophile
East Germany (German Democratic Star Republic): Conformist
– Despotic Hegemony
– Materialist, Collectivist, Xenophobe
Russia (Russian Cosmosphere): Adaptive
– Despotic Hegemony
– Fanatic Materialist, Collectivist
Soviet Russia (Union of Soviet Star Republics): Resilient, Natural Physicists
– Fanatic Collectivists, Materialist
– Despotic Hegemony
The belfry (gamez7) mac os. Brazil (Regime Militar do Brasil): Adaptive, Agrarian, Sedentary, Slow Learners
– Military Junta
– Xenophile, Spiritualist, Militarist
Scullys morning mac os. Indonesia (Union of Javan Suns): Nomadic, Rapid Breeders
– Individualist, Xenophile, Spiritualist
– Indirect Democracy
France (Sixth Republic): Adaptive, Fast Breeders, Sedentary
– Indirect Democracy
– Individualist, Materialist, Militarist
England (Anglian Star Empire): Talented, Natural Physicists, Solitary.
– Enlightened Monarchy
– Pacifist, Fanatic Materialist
Scotland (Assembly of Alba): Thrifty
– Xenophile, Pacifist, Spiritualist
– Moral Democracy
Mexico (Mexican Empire): Nomadic, Communal
– Spiritualist, Militarist, Xenophile
– Military Junta
Italy (Roman League): Nomadic, Slow breeders, Communal
– Plutocratic oligarchy
– Spiritualist, Xenophile, Pacifist
South Korea (Korean Conglomerate): Industrious.
– Plutocratic Oligarchy
– Fanatic Materialist, Militarist
Saudi Arabia (Unified Clans of Arabia): Decadent, Nomadic, Agrarian
– Divine Mandate
– Fanatic Spiritualist, Militarist
Canada (Confederation of Canadia): Natural Sociologists, Charismatic
– Moral Democracy
– Fanatic Pacifists, Xenophile
Turkey (Turkish Sovereign Republic): Nomadic, Communal
– Theocratic Republic
– Spiritualist, Xenophobe, Militarist
Australia+NZ (Anzac Confederacy): Nomadic, Resilient, Charismatic, Solitary
– Indirect Democracy
– Individualist, Xenophobe, Militarist
Argentina (La Plata): Agrarian
– Military Republic
– Individualist, Militarist, Xenophobe
South Africa (South African Pact): Industrious, Resilient, Solitary
– Military Junta
– Collectivist, Militarist, Xenophobe
Spain+Portugal (Iberian Union): Communal, Charismatic
– Indirect Democracy
– Xenophile, Pacifist, Spiritualist
Friends:
Balkan Nations (Balkan Bloc): Agrarian, Strong, Slow Breeders
– Collectivist, Militarist, Spiritualist
– Military Junta
Netherlands+Flanders (United Netherlands):Thrifty
– Xenophile, Pacifist, Materialist
– Enlightened Monarchy
Scandinavia (Nordic Council): Natural Sociologists, Talented, Weak
– Moral Democracy
– Fanatic Pacifist, Xenophile
Israel (Children of Zion): Thrifty, Strong, Solitary
– Militarist, Spiritualist, Xenophobe
– Military Republic
Nigeria/Black Africa (African Union): Nomadic, Rapid Breeders
– Xenophile, Militarist, Spiritualist
– Indirect Democracy
North Korea (Korean Democratic Stars): Industrious, Resilient, Solitary
– Fanatic Collectivist, Militarist
– Despotic Empire
Singapore (Singapore Technate): Intelligent
– Science Directorate
– Fanatic Materialist, Individualist
Switzerland (Helvetian Interstellar Confederation):
– Direct Democracy
– Materialist, Xenophobe, Militarist
The Cosmosphere Of Armastus Mac Os Catalina
Ireland (Irish Diaspora): Charismatic, Nomadic, Rapid Breeders, Nonadaptive
– Moral Democracy
– Pacifist, Xenophile, Materialist
Mars does have an atmosphere, though some of it has been lost over the course of billions of years. The planet has become evidence of large-scale climate change, losing much of its once-thick atmosphere to having one 100-times thinner than that on Earth, with about 1% of its density. Scientists continue to study the composition of the planet's atmosphere and its volume to determine whether there may once have been life on the fourth planet from the sun, and if it could ever sustain life as we know it again.
What Is The Martian Atmosphere Made Of?
Martian atmosphere is comprised mainly of carbon dioxide (95%). The remainder of the elements are nitrogen (2.7%), argon (1.6%), oxygen (0.13%), carbon monoxide (0.08%), and minor levels of water, nitrogen oxide, neon, hydrogen-deuterium-oxygen, krypton, and xenon.
Carbon dioxide makes up the greatest portion of the Martian atmosphere. The planet becomes so cold in winter months, carbon dioxide ice caps form on the poles but when they are exposed to heat those caps undergo sublimation and return to gas form. Because carbon dioxide transforms from gas to solid form regularly, the atmospheric composition can change from year to year as the element condenses or sublimes. The levels of carbon dioxide on the Red Planet exceed those on Earth due to a lack of plant life, which helps convert the carbon dioxide into oxygen.
Though it accounts for just 2.7% of the atmosphere on Mars, many scientists believe there may be higher levels of nitrogen on the planet as some of it may be hidden and stored as nitrate salt within the planet's red soil. Those amounts of solid nitrogen have not been measured, however.
There is more argon in the atmosphere of Mars than any other planet, and its levels are constant because the gas does not condense. Despite its actual amounts remaining steady, the relative levels of argon in the atmosphere may fluctuate as carbon dioxide moves in and out of the atmosphere via condensation.
What Is Mars Like?
The Red Planet is a cold, desert-like environment with dry riverbeds and minerals that form only with liquid water. These elements of the planet's make-up lead scientists to believe Mars once had a thick enough atmosphere to retain heat, which would have permitted water to flow on its surface similar to Earth. As the atmosphere faded, the climate of Mars transformed into a frozen and dessicated land, and water is scarce or non-existent. It's atmosphere is now so thin, it could not sustain life.
With a thin atmosphere and its distance from the sun, the Red Planet is cold, with average temperatures hovering around -80 degrees Fahrenheit or -60 degrees Celsius and notable cold snaps reaching -195 F (-125 C) near the poles and midday heat climbing to 70F, or 20C, near its equator.
The Cosmosphere Of Armastus Mac Os 7
How Was The Atmosphere Lost?
It is difficult to estimate just how much of Mars' atmosphere was lost, because scientists are unable to solve the mystery of how thick it was in ancient times. While studies indicate it was healthy enough to keep the planet warm and water flowing, there is no evidence as to just how much atmosphere Mars once had.
The Cosmosphere Of Armastus Mac Os X
Scientists have looked at isotopes of oxygen on the planet for some clue. Lighter isotopes escape into space faster than heavier ones, and the Red Planet has rich levels of heavier oxygen isotopes. These amounts can help estimate how much more atmosphere once existed if scientists work with the assumption the amounts of light and heavy oxygen isotopes on Mars were once similar to Earth.
Some believe the atmosphere may have been compromised by a devastating impact from a small body, which could have stripped way many isotopes and left behind a thinner atmospheric layer.
Leading theories for the reason of atmosphere loss is that the planet's light gravity and lack of a magnetic field left its ancient atmosphere susceptible to pressure from strong solar winds, which carry a consistent stream of particles from the sun. Pressure from the sun pulled lighter isotopes from the atmosphere, thinning it out.
In 2013, NASA's MAVEN mission measured the rate Mars' atmosphere was being stripped away by solar winds, which would have provided data to infer the rate it had lost the rest of its atmospheric layer through history. Dragon ball z: run! mac os. The findings indicated Mars loses approximately 100 grams, or 0.25 pounds, of its atmosphere every second. When solar flares occur, that rate increases by about 20 times. Scientists estimate when the atmosphere was at its thickest, the same levels of solar winds would have stripped it away faster.
What Is The Importance Of The Martian Atmosphere?
The atmosphere on Mars may be much thinner than on Earth, but it remains intact enough to cause weather, clouds, and wind. Often during spring and summer, weather patterns cause giant dust devils, kicking up the oxidized iron dust that covers its surface, giving Mars its signature red hue. One theory as to the cause of the dust storms is that the airborne particles, which are considered a permanent part of the atmosphere, absorb sunlight and cause warmer pockets of air to flow through cold regions, which generates strong wind. These winds lift more dust from the ground into the air, heating the atmosphere more, creating more wind and dust.
The high levels of carbon dioxide in the atmosphere create Martian snowflakes, which are actually small particles that form together and create a fog-like effect. The planet's poles are also covered in ice caps, but these are also largely comprised of carbon dioxide rather than water.
