
Super-Earth GJ1214b orbits a red dwarf star (artist’s view).
Over the past year there has been a string of breathless news stories about astronomers finding extrasolar planets in the habitable zone around their star. This is the “Goldilocks zone” where temperatures are not too hot, and not too cold, but just right for surface water to remain liquid and presumably nurture life as we know it.
Astronomers with the Search for Extraterrestrial Intelligence (SETI) are firing up their Allen Array telescope to check out these worlds for signs of intelligent life.
But using the term Earth-like for these planets is stretch at best, and misleading at worst. We don’t have a clue about the physical nature or processes on these worlds, any more than an air traffic control radar blip tells you what meals are being served on a commercial flight.
Saying that water could exist is OK, but to imply it does exist with the phrase “Earth-like planet” is very presumptive.
The bottom line is that we don’t know how Earth got tanked-up with its water supply. So how might we guess what’s happening on worlds thousands of light-years away?
“If we need exotic mechanisms to get water onto Earth, then maybe it suggests life is not prevalent in these exoplanetary systems,” says astrobiologist Karen Meech of the University of Hawaii.
The oceans account for merely one-quarter of one percent of Earth’s mass. Another one-tenth of a percent of water may be in Earth’s mantle. If we could probe deeper, down into the core, Earth could conceivably have 50 oceans worth of water locked away from the days of our planet’s formation. (This is somewhat bemusing, considering Jules Vern wrote about a great subterranean ocean in the 1864 “A Journey to the Center of the Earth.”)
With water potentially so locked away, “we may never know how much water Earth really has,” says Meech.
This complicates several competing theories for how Earth got its water supply in the first place. We know water is everywhere in the solar system, especially among the planets and moons of the outer solar system. They lie beyond the “frost line” where water can remain a solid. By comparison, the baked, rocky planets Mercury and Venus seem bone-dry, and Mars looks arid at best.
From the geologic record we do know that oceans were here on Earth just a few hundred million years after our planet’s formation 4.6 billion years ago.
Recent computer simulations show that all hell would have broken loose in our solar system if the outer planets had ever migrated in their orbits – a phenomenon commonly seen in exoplanetary systems that may also have happened here. Earth would have been pelted with water-bearing asteroids that were thrown into Earth-crossing elliptical orbits. This would explain a late, heavy asteroid bombardment 3.9 billion years ago, as recorded on the moon and other solar system bodies.
Or perhaps water was transported to the early Earth by a class of object that no longer exists? And did the water appear late, early or in intermediate episodes in Earth’s formative years?
The picture is so complicated that it’s safest to say that water came to Earth from many sources: comets, hydrated asteroids, solar nebula gasses, and chemical processing on Earth’s surface.
Because we don’t even know how much water Earth has, we don’t know if our planet is a comparatively dry or wet planet. Now astronomers using Hubble have found a new class of planet that may truly be a water world. Zachory Berta of the Harvard-Smithsonian Center for Astrophysics (CfA) and colleagues have uncovered a new class of planet where a very large fraction of its mass is water. A thick, steamy atmosphere enshrouds it. But don’t plan on going surfing; the surface temperature is 450 degree Fahrenheit.
The waterworld, called GJ1214b, is 2.7 times Earth’s diameter and orbits a red dwarf star every 38 hours at a distance of 1.3 million miles.
In 2010, CfA scientist Jacob Bean and colleagues reported that they had measured the atmosphere of GJ1214b, finding it likely that the atmosphere was composed mainly of water. However, a hazy atmosphere could also explain their observations.
The infrared capabilities of Hubble’s Wide Field Camera 3 were used to study the planet at infrared wavelengths when it passed in front of its star. The team essentially used Hubble to measure the infrared color of sunset on this world. Hazes are more transparent to infrared light than to visible light, so the Hubble observations help tell the difference between a steamy and a hazy atmosphere.
The astronomers found the spectrum of GJ1214b to be featureless over a wide range of colors. The atmospheric model most consistent with the Hubble data is a dense atmosphere of water vapor.
The planet could only have amassed so much water if the planet had formed farther away from its star, beyond the frost line where water ice would be abundant. The planet then migrated inward toward the star, either through friction with gas in the disk or by gravitational interactions with other planetary bodies.
In the process, the wandering planet would have passed through the star’s habitable zone. Therefore, long ago it would have had a balmy ocean like Earth’s. But was the planet there long enough for life to start? The water planet is a prime candidate for further observations with the infrared capabilities of the upcoming James Webb Space Telescope.