Hunters of alien life may have a new and unsuspected niche to scout out.
A recent paper submitted by Associate Professor of Astronomy at Columbia University Kristen Menou to the Astrophysical Journal suggests that tidally-locked planets in close orbits to M-class red dwarf stars may host a very unique hydrological cycle. And in some extreme cases, that cycle may cause a curious dichotomy, with ice collecting on the farside hemisphere of the world, leaving a parched sunward side. Life sprouting up in such conditions would be a challenge, experts say, but it is — enticingly — conceivable.
The possibility of life around red dwarf stars has tantalized researchers before. M-type dwarfs are only 0.075 to 0.6 times as massive as our Sun, and are much more common in the universe. The life span of these miserly stars can be measured in the trillions of years for the low end of the mass scale. For comparison, the Universe has only been around for 13.8 billion years. This is another plus in the game of giving biological life a chance to get underway. And while the habitable zone, or the “Goldilocks” region where water would remain liquid is closer in to a host star for a planet orbiting a red dwarf, it is also more extensive than what we inhabit in our own solar system.
![Gliese 581- an example of a potential habitable zone around a red dwarf star contrasted with our own solar system. (Credit: ESO/Henrykus under a Wikimedia Creative Commons Attribution 3.0 Unported license).](https://www.universetoday.com/wp-content/uploads/2013/07/Gliese_581_-_2010-580x395.jpg)
But such a scenario isn’t without its drawbacks. Red dwarfs are turbulent stars, unleashing radiation storms that would render any nearby planets sterile for life as we know it.
But the model Professor Menou proposes paints a unique and compelling picture. While water on the permanent daytime side of a terrestrial-sized world tidally locked in orbit around an M-dwarf star would quickly evaporate, it would be transported by atmospheric convection and freeze out and accumulate on the permanent nighttime side. This ice would only slowly migrate back to the scorching daytime side and the process would continue.
Could these types of “water-locked worlds” be more common than our own?
The type of tidal locking referred to is the same as has occurred between the Earth and its Moon. The Moon keeps one face eternally turned towards the Earth, completing one revolution every 29.5 day synodic period. We also see this same phenomenon in the satellites for Jupiter and Saturn, and such behavior is most likely common in the realm of exoplanets closely orbiting their host stars.
The study used a dynamical model known as PlanetSimulator created at the University of Hamburg in Germany. The worlds modeled by the author suggest that planets with less than a quarter of the water present in the Earth’s oceans and subject to a similar insolation as Earth from its host star would eventually trap most of their water as ice on the planet’s night side.
Kepler data results suggest that planets in close orbits around M-dwarf stars may be relatively common. The author also notes that such an ice-trap on a water-deficient world orbiting an M-dwarf star would have a profound effect of the climate, dependent on the amount of volatiles available. This includes the possibility of impacts on the process of erosion, weathering, and CO2 cycling which are also crucial to life as we know it on Earth.
Thus far, there is yet to be a true “short list” of discovered exoplanets that may fit the bill. “Any planet in the habitable zone of an M-dwarf star is a potential water-trapped world, though probably not if we know the planet possesses a thick atmosphere.” Professor Menou told Universe Today. “But as more such planets are discovered, there should be many more potential candidates.”
![Hard times in harsh climes-an artist's conception of the daytime side of a world orbiting a red dwarf star.](https://www.universetoday.com/wp-content/uploads/2013/07/344828main_image_1347_946-710-580x435.jpg)
Being that red dwarf stars are relatively common, could this ice-trap scenario be widespread as well?
“In short, yes,” Professor Menou said to Universe Today. “It also depends on the frequency of planets around such stars (indications suggest it is high) and on the total amount of water at the surface of the planet, which some formation models suggest should indeed be small, which would make this scenario more likely/relevant. It could, in principle, be the norm rather than the exception, although it remains to be seen.”
Of course, life under such conditions would face the unique challenges. The daytime side of the world would be subject to the tempestuous whims of its red dwarf host sun in the form of frequent radiation storms. The cold nighttime side would offer some respite from this, but finding a reliable source of energy on the permanently shrouded night side of such as world would be difficult, perhaps relying on chemosynthesis instead of solar-powered photosynthesis.
On Earth, life situated near “black smokers” or volcanic vents deep on the ocean floor where the Sun never shines do just that. One could also perhaps imagine life that finds a niche in the twilight regions of such a world, feeding on the detritus that circulates by.
Some of the closest red dwarf stars to our own solar system include Promixa Centauri, Barnard’s Star and Luyten’s Flare Star. Barnard’s star has been the target of searches for exoplanets for over a century due to its high proper motion, which have so far turned up naught.
The closest M-dwarf star with exoplanets discovered thus far is Gliese 674, at 14.8 light years distant. The current tally of extrasolar worlds as per the Extrasolar Planet Encyclopedia stands at 919.
This hunt will also provide a challenge for TESS, the Transiting Exoplanet Survey Satellite and the successor to Kepler due to launch in 2017.
Searching for and identifying ice-trapped worlds may prove to be a challenge. Such planets would exhibit a contrast in albedo, or brightness from one hemisphere to the other, but we would always see the ice-covered nighttime side in darkness. Still, exoplanet-hunting scientists have been able to tease out an amazing amount of information from the data available before- perhaps we’ll soon know if such planetary oases exist far inside the “snowline” orbiting around red dwarf stars.
Read the paper on Water-Trapped Worlds at the following link.
I’m sure there would be ample liquid water at the day-night terminator. And the area might be quite large if the planet’s orbit is at all eccentric (compare the moon’s wobble). Though the weather would probably be rather extreme.
There could also be seasonal effects if the planet has a substantial axial tilt.
If the planet is tidally locked then there is no axis of rotation with respect to the host star. So no axial tilt. Wobble could cause seasonal effects.
Such planets should divide up into 3 regions: A hot dry zone facing the star in permanent sunshine, The terminator zone which would be temperate, and a frigid and snowy zone in permanent darkness, likely with an ocean covered with a thick layer of ice. I have concerns about a static hydrological cycle developing, however. Once water vapor freezes out an precipitates on the dark side, what process will recycle it back? Without rotation or seasons, I don’t see a process that would melt frozen moisture from the cold dark side to get it back to the temperate or warm zones. Such planets would be relatively easy to terraform for human habitation, however, simply by digging canals, creating meltwater with furnaces and using solar powered pumps to move water to sunlit areas.
After putting some thought into this, I came of with the following hypothesis: Such planets would essentially function as if they have a single hemisphere. The equator would be the portion of the planet that always faces the sun. On the other end would be essentially a polar ice cap in permanent darkness. The sharp temperature gradient would drive strong convection currents (winds) in a polar direction. There would also be zonal wind flows perpendicular to these. So the night side would be warmed enough to melt ice and presumably create a hydrologic cycle. The subpolar regions, also in permanent darkness, would be wet and very stormy. Meltwater should reach the temperate region in the form of lakes and rivers. The climate would become progressively drier and warmer closer to the “equator” where there is the most direct sunlight.
It’s possible that while most water becomes trapped on the night side of such planets, the atmsphere continues to circulate, and will melt a portion of the nightside glacier, much like glaciers both melt and accumulate icia via freezing on Earth.
It would be interesting to see a list of red dwarf stars visible in amateur telescopes? Do you know of one? The Harvard Smithsonian Center for Astrophysics site says there are no red dwarf stars visible to the naked eye… but how small a telescope is needed to see one?
Great idea; while there are no red dwarfs visible to the unaided eye from the Earth, there are several in the +8 to 12 magnitude range, including Groombridge 34 & Luyten’s Flare Star. One of our faves is Omicron Eridani, which is a fine example of a K-type main sequence star paired up with a white & red dwarf visible with a backyard telescope;
http://astroguyz.com/2009/11/30/astro-challengespy-a-white-dwarf/
Thanks Dave! I have put your suggestions in my list of future observations. I generally use a 4″ S/C and should be able to see these stars. The Kepler planet-hunting mission suggests that about 6 percent of red dwarfs should have habitable planets, which further suggests there could be as many as 60 billion habitable planets orbiting red dwarfs in our galaxy! For what it’s worth… the description of beings from assumed alien encounters have often been depicted with small wiry bodies with very large eyes – possibly indicating they have come from low mass planets orbiting red dwarf stars?
For those interested:
Groombridge 34 is approx. 11.6 ly away, in Andromeda @ 0h18m22.9s, 44*01’22.6″ mag. 8-11
Luyten’s flare Star is approx. 8.7 ly away, in Cetus @ 01h39m1.54s, -17*57’1.8″ mag. 12.57
DY Eridanus is approx. 16.5ly away, in Eridanus @ 4h15m3s, -7*39′ mag. 11
Interesting. Such finds of habitable environments makes me more optimistic about M dwarfs habitability.
Not all M dwarfs are turbulent though, and while the frequency goes up for small stars the flare stars are still constrained to be in the percent range (AFAIK).
Another interesting development is the identification of various dichotomy classes among the small period planets.
There is a statistically significant division between rocky planets of less than ~ 2 Earth radii and others above.
And there is a division between small transit rocky planets ~ 10 Earth masses (~2 Earth radii) and large transit rocky planets with a ~ 1 % hydrogen atmosphere by mass and ~ twice the radius. The latter dichotomy seems to be caused by x-ray erosion of the atmosphere, meaning that stars that integrates up “radiation storms” to atmosphere damage over their early billions of years can perhaps be easily detected. [Both talks from IAU299.]
[The embedded figures seems to be UT functionality. Niftily, the “expand” tool takes me to a fullscreen video]
if there is a permanent dark and light side then there must be a permanent twilight in between
SInce huge amount of water is trapped on the dark side of the planet carbon dioxide have to collect in the atmosphere causing greenhouse effect