Sun’s Habitable Zone
Overview
Note
See this section’s top page for some background on the Sun.
A habitable zone is the region around a star where liquid water could exist on the surface of a planet.
Defining these zones requires a lot of assumptions about the planet’s host star and the planet itself. For one, we are assuming a terrestrial-like planet. One with an favorable atmosphere for life. It factors in greenhouse effects, intensity of light from the star, atmospheric composition, and other parameters.
Inner, Red Edge
The inner, red, edge of the zone is characterized by a runaway greenhouse limit, where the oceans would vaporize completely. Venus, for example, touches the inner edge of the Sun’s habitable zone. The planet could, and likely once did, support water given its surface pressure, but its greenhouse effect raises the surface temperature to over 400°C (over 800°F), vaporizing any liquid water.
Outer, Blue Limit
The outer, blue, edge of the zone is largely determined by the incident solar light on the planet and the ability of the planet to absorb it. Here, we have a maximum amount of warming possible, resulting in a “freezing out” of the atmosphere beyond the zone.
Mars
Mars is closer to the outer edge, and has a lower atmospheric pressure and temperature. Only at its lowest elevations and during the part of the year when temperatures rise above freezing on the surface could liquid water exist for a short period of time.
Water Beyond the Habitable Zone
Astronomers have discovered liquid water beyond this zone, notably in Jupiter’s moons Europa and Ganymede and Saturn’s moons Titan and Enceladus—all well outside this habitable zone for the Sun. These favorable conditions may result from tidal heating (when a body is being stretched or squeezed by a larger, nearby body) or radioactive decay (unstable elements decay and produce energy in the form of heat).
Profiles
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Habitable Zones Around Main-Sequence Stars—Dependence on Planetary Mass |
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