Exoplanets 101: Does the earth have a twin?

potential habitatable planets

Potential Habitable Planets

An extrasolar planet is a planet that orbits a star that’s not our sun. Even though these planets can be recognized, and their sizes measured, they are light years away so it would take astronomers thousands of years to reach these extrasolar planets. To detect these planets, scientists use either one of two methods: doppler and transit.

The doppler method measures the star’s wobble. The wobble is caused by the force of gravity from exoplanets themselves, pulling the stars in different directions during their orbits. Measuring the wobble also makes it possible for astronomers to measure the planet’s mass. The greater the wobble of the star, the greater the mass of the exoplanet.

The transit method: after observing a star over a period of time, astronomers sometimes notice a faint dimming of its light. This dimming is probably caused by a planet orbiting past it. Taking note of the “size of the dim” through the transit method gives away the size of the planet. The doppler technique gives astronomers the mass of the exoplanet, and the transit method gives them the radius/physical size.

Combining the results, astronomers are able to calculate the density of the exoplanet. The value of the density of the planet is then used to determine the kind of planet that has been discovered. Ie, is it a rocky planet like earth or a gaseous, giant planet like Jupiter? A gas giant like Jupiter has a low density, and a rocky metallic planet like earth has a high density.

What will it take to find a planet like earth? There is a difference between being earth-sized and being earth-like. Astronomers have discovered hundreds of planets that may be the same size as our earth but a planet must be at the right distance from its  star, to have the right conditions where liquid water could exist on its surface. We are not entirely sure of what the atmospheres on these earth-like planets may be like, or whether these earth-like planets actually have atmospheres but we are excited to discover what could be our very own twin planet!

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Europa

Europa, a moon of the planet Jupiter, was discovered in 1610 by Galileo Galilei and Simon Marius. It is a little smaller than Earth’s moon, and it has one of the smoothest surfaces in the solar system. The surface is made up of water ice with long, linear lines fracturing it. The low number of craters and cracks suggest that the surface is no more than 40 million to 90 million years old. There is the possibility that Europa has an iron core and a frozen ocean beneath the crust. No concrete evidence for this ocean exists yet, but previous missions have made it possible to strongly suggest its existence. Tides, which occur because of Jupiter’s stronger gravity on the near side Europa, have been observed, and if the ocean exists these tides could create hydrothermal activity that could make the ocean fit for living things.

Europa
Source: NASA – The trailing hemisphere of Europa. The right image is an enhanced false-color composite.

It takes about 3.5 Earth days for Europa to complete a rotation of its axis. This is also the amount of time it takes for Europa to elliptically orbit Jupiter. The average orbit velocity of this moon is about 46% of Earth’s. The surface temperature is about 110 K on average at the equator and 50 K at the poles. These low temperatures keep the crust solid. Europa’s atmosphere is made up of mostly oxygen as well, however it is very thin. Galileo, the spacecraft, confirmed the presence of an atmosphere when it discovered a weak atmospheric layer of charged particles in 1997. The oxygen in Europa’s atmosphere did not originate there either. Ultraviolet radiation and charged particles smash into Europa’s surface, which splits the water molecules into oxygen and hydrogen atoms that are absorbed into the atmosphere. This ongoing process is referred to as radiolysis.

Image result for europa clipper
Source: NASA – Artist conception of Europa Clipper in orbit

NASA’s Europa Clipper plans to launch in 2023, and will orbit Jupiter in order to carry out flybys of the moon and investigate its structure and contents. Learn more about the mission here!

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Probing the Mysteries of 50000 QUAOAR

Hundreds of millions of miles beyond the orbit of Neptune lurks one of the most intriguing objects in the Solar System, 50000 Quaoar.

The Mighty 50000 Quaoar

50000 Quaoar is notable for multiple reasons, but the most apparent is its name. Quaoar is the name of the creator deity of the Tongva people in the Los Angeles Basin. The deity Quaoar was believed to have control of a group of “avengers” who spied on humanity and enforced Quaoar’s will. While 50000 Quaoar certainly has an impressive namesake, the 50000 portion is also interesting from an astronomical point of view.

Ordinarily, Solar System objects will be named along with a number denoting how many similar objects had been found before. For instance, 1154 Astronomia was the 1154th minor planet found in the solar system. This chart has all of the minor planets found in order. But for a Solar System object as interesting as Quaoar, scientists decided to break entirely with this tradition to give it a number more fitting to its power; thus we have 50,000 Quaoar.

Another interesting fact concerning Quaoar is that it is a cubewano, and despite the fact that WordPress has underlined it in red on my screen, this strange term cubewano is really an English word. It comes from the provisional name of trans-Neptunian object 15760 Albion, 1992 QB1. 1992 QB1 was left unnamed for over two decades, so whenever another trans-Neptunian object was located it was named after this provisional name (if you say QB1 fast enough it begins to sound like cubewano).

Cubewanos are often very large. The largest of them Makemake is actually a dwarf planet, although this isn’t unique to Makemake. 50000 Quaoar may also be a dwarf planet, and it even has its own 50 km moon, Weywot.

50000 Quaoar looking menacing

Some scientists have hypothesized that 5000 Quaoar was originally much larger and collided with another trans-Neptunian object, possibly even Pluto. Quaoar has also been chosen as a target for a flyby in the 2030s, so get your tickets soon.

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Hypothetical Planets in the Kuiper Belt and Oort Clout

               With all the data we have on the orbits of familiar objects of our solar system, some interesting hypothesis have been formed about large bodies within or beyond the Kuiper Belt. This method of discovery was used in the 1840s to discover Neptune by studying the orbit of Uranus and noticing then compensating for gravitational irregularities. In 1999 a similar prediction was made for a hypothetical gas giant situated far from the sun in the Oort cloud (1), based on the trajectories of incoming comets. While Tyche’s existence has been disproved by astronomical surveys, another potential body may exist in the Kuiper Belt which has not yet been disproved. This hypothetical Planet 9 compensates for the aligned orbits of a handful of significant Kuiper Belt Objects, as illustrated in figure 1 (2). While it remains elusive from our telescopes, current technology can not rule out the predicted Neptunian sized object.

Figure 1: Showing the potential orbit of the hypothetical Planet Nine, with other KBOs

Sources:

  1. https://en.wikipedia.org/wiki/Tyche_(hypothetical_planet)
  2. https://www.nature.com/news/evidence-grows-for-giant-planet-on-fringes-of-solar-system-1.19182


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Ultima Thule

The New Horizons space probe was launched in 2006—primarily to study Pluto, but also to study Kuiper belt objects in its following years. Following the space probe’s flyby of Pluto in 2015, it reached 2014 MU69, also known as Ultima Thule, on January 1, 2019. Ultima Thule is a Kuiper belt object that orbits 1.6 billion kilometers beyond Pluto, making it the farthest object that has been visited by a spacecraft. That being said, it will take approximately 20 months for all the data gathered by the New Horizons probe to be sent to Earth, and all the data won’t be back until the summer of 2020. Here’s some of what we do know: The object is a “contact binary” made of two planetesimals that have been fused together, nicknamed “Ultima” and Thule.” It is approximately 31 kilometers long and has a red surface color. The two parts of the object seem to have orbited one another until they were merged together. New Horizons observations have shown that Ultima—the larger lobe—is flattened, and the smaller lobe—Thule—is more rounded, like a walnut. The unique shape of this object is unlike anything else that has been seen in the solar system so far, and it allows us to look into the earliest stages of planetesimal accretion and planet formation within our solar system.

New Horizons image of 2014 MU69 (Ultima Thule) – By NASA/Johns Hopkins Applied Physics Laboratory/Southwest Research Institute, National Optical Astronomy Observatory, Public Domain
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Io

Io

Io is one of the closest and most prominent of Jupiter’s moons. Surprisingly, Io has the most volcanic activity of any of the worlds in our solar system. Usually, people think of moons as large barren rocks (similar to our own) however, Io breaks that mold. Because Io has such a large amount of volcanoes, we know that its internal temperature must be pretty high. This high internal temperature is due to tidal heating. Jupiter exerts a great tidal force on Io due its large mass. This large tidal force added to the fact that Io’s orbit around Jupiter is somewhat elliptical means that the size and orientation of Io’s tidal bulges are constantly changing. The changing in these tidal bulges causes Io to experience a lot of internal friction, which is what makes Io have a very hot interior. Not only is Io’s internal temperature what makes it interesting, the fact that it has a slightly elliptical orbit adds to its uniqueness. Typically, a moon or other large body of Io’s size would have a nearly circular orbit. However, due to the gravitational tug between Io and Jupiter’s other large moons, Io is moved into an elliptical orbit.

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Eight Planets or Nine?

Most of us probably remember a time when the Solar System had nine planets, with Pluto as the ninth and (usually) farthest from the Sun. In 2006, following the discovery of Eris, the International Astronomical Union (IAU) voted to reclassify Pluto as a “dwarf planet” (don’t forget the quotation marks!). However, there might one day be a ninth planet yet again!

Artist’s conception of Planet Nine with the Sun and Milky Way in the background
Source: Nagualdesign and Tom Ruen via Wikimedia Commons

Astronomers have been searching for a possible Planet Nine beyond Neptune’s orbit ever since 2004, when the peculiarity of Sedna’s orbit was discovered. Sedna’s orbit (76 AU at perihelion) is farther out than can be explained by gravitational interactions with Neptune alone, hinting at an interaction with an unknown object. Ten years later, a similar case was discovered: another dwarf planet orbiting at 80 AU, too far to be explained solely by Neptune’s gravity. 

Even more recently, in 2016, two scientists from the California Institute of Technology (Caltech), Konstantin Batygin and Mike Brown, proposed a detailed hypothesis for the existence and characteristics of Planet 9. According to them, Planet Nine has the following characteristics:

  • Its perihelion distance is probably around 200 AU, but could be up to 350 AU.
  • Its aphelion distance (which is harder to determine) is between 500 AU and 1200 AU.
  • Its mass is at least 5x that of Earth, but likely around 10x or possibly greater
  • Its radius is about 2x-4x that of Earth
  • Its appearance is similar to that of Neptune

Notice that this proposed Planet 9 is incredibly far away! For reference, Earth orbits (by definition) at a distance of 1 AU, while Neptune orbits at around 30 AU. Considering that Planet 9 is around ten times farther from the Sun than Neptune (which we already cannot see with the naked eye), it is not surprising that we have not yet been able to detect this planet. Furthermore, it is quite probable that Planet 9 is currently at aphelion, making detection even more difficult (especially due to the Milky Way Galaxy in the background), considering that it would likely be fainter than a 22nd magnitude star. However, a number of powerful sky surveys have ruled out areas where Planet 9 isn’t, and hopes are high that in the near future, more survey data will be able to pinpoint the location of this mysterious planet! If so, I feel it will be one of the most exciting astronomical discoveries in our lifetime!

Do you think there’s a planet Nine out there?

Sources:

“Planet Nine.” Wikipedia, Wikimedia Foundation, 28 Mar. 2019. Web.

Batygin, Konstantin, and Mike Brown. “The Search for Planet Nine.” The Search for Planet Nine, 1 Jan. 1970. Web.

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Extrasolar Planets: A Search to Span Solar Systems

Recently, I have started work as an undergraduate research assistant in the Physics and Astronomy department at my university. The project I was assigned to is of a stellar nature; we are attempting to find evidence of extrasolar planets, or planets around other stars. Though we haven’t found any planets yet, I keep thinking about how crucial this type of work is to the future of the human race. Around 4,000 extrasolar planets have been confirmed by NASA, and it is amazing to think that one of these could be humanity’s next home. In this blog post, I will discuss the major approaches that astronomers use to detect planets outside of our solar system.

The Astrometric Method: Using the astrometric method, we can detect extrasolar planets by carefully monitoring small changes in the host star’s position in the sky. Planets orbit their host stars because of the enormous amount of gravitational force exerted on them by their stars. However, the laws of physics tell us that the planets also exert an equal amount of gravitational force on their host star. Though the star is much more massive, the planets can cause a star to “wobble” as it is gravitationally tugged at. Very few extrasolar planets have been identified using this method; the star studied must be relatively near to us, and observing positional changes may require long periods of observation.

Image Source: Wikipedia

The Doppler Method: Like the astrometric method, the Doppler method relies on the gravitational interactions and “tugs” between a host star and its planets. When a star is moving towards or away from us, we say that its light spectrum is blueshifted or redshifted, respectively. Alternating blueshifts and redshifts relative to average Doppler Shift can indicate a star’s motion or “wobble” due to its interactions with a planet or planets. The Doppler method has discovered many more extrasolar planets than the astrometric method, but it certainly does not come without its limitations. This technique is best suited for massive planets with close orbits, and because it calls for stellar spectra, large telescopes and long periods of observation are a must.

Image Source: EarthSky

The Transit Method: When an extrasolar planet’s orbital plane is situated along our line of sight, the planet will appear to travel in front of its star once every orbit. Astronomers call this a transit event. Similarly, half an orbit later, the planet will become eclipsed by its host star as it passes behind. We can detect these events by monitoring changes in the star system’s brightness. During a transit event, the star undergoes a characteristic dip in brightness as the planet blocks some of its light. During an eclipse, there is a dip in the system’s infrared brightness as the star blocks the infrared light emanating from the planet. Most extrasolar planets have been discovered using this method, but it is only feasible for planets with orbital paths that are oriented in just the right way.

Image Source: National Aeronautics and Space Administration

Direct Detection: This technique involves acquiring images or spectra of the planet. In theory, this is the best way to learn about an extrasolar planet; however, our current technology can only produce images with low resolution. There are other obstacles to directly detecting planets as well. For one, stars give off much more light than any planets that might be orbiting them. Because of diffraction, our telescopes also blur star light. Most extrasolar planets are too close to their bright host stars to be imaged directly from our vantage point, light years away. Second, compared to massive stars and the colossal distances between them, planets are miniscule.

An infrared image of a brown dwarf and an extrasolar planet (bottom left corner) located about 230 light years from Earth. Image Source: Slate
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Halley’s Comet

In 2061, Halley’s Comet will return to pass by Earth in 75-year long round trip across the solar system. But what else do we know about this mysterious visitor?

Studying the reports of comet sightings in 1531, 1607, and 1682, Edmond Halley deduced that these comets were in fact the same one and that it would return in 1758. Though Halley died in 1742, the comet did indeed return in 1758 and was named after its discoverer. When Halley’s comet returned in 1986, technology had finally allowed astronomers to study it. Probes from multiple international space programs were sent take close-up pictures of the comet for the first time. Research has shown that Halley’s comet is slowly losing about a thousandth of its mass with every loop around. Although it will still take thousands of years to finally die out, it is disheartening to see that not all things in the universe are permanent.

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Enceladus

The Surface of Enceladus, captured by the Cassini spacecraft
Source: NASA via Wikipedia

Enceladus is a medium-size moon of Saturn, with a diameter of about 500 km. Its surface temperature is quite chilly, ranging between 32.9 K (-240 degrees Celsius) and 145 K (-128 degrees Celsius); this is partially because of its distance from the Sun, and also because of its highly reflective surface. The entire moon is coated in fresh ice, so it reflects a lot of the sunlight that reaches it. This helps make it cold, and also makes it one of the brightest worlds in the solar system. Despite its small size and its frigid surface temperatures, Enceladus seems to show signs of ongoing geological activity, due to the fact that its orbital resonance with Dione (another of Saturn’s moons) causes tidal heating.

One of the most fascinating things about Enceladus is that it is believed to have a global subsurface ocean of water beneath its coating of ice. Thanks to tidal heating, Enceladus spews geysers of its ocean material from near its South Pole. The Cassini spacecraft found that these geysers contain mostly water vapor, along with traces of nitrogen, methane, and carbon dioxide. The geysers reach hundreds of miles into space, and the released material makes up most of Saturn’s E ring.

Cassini image of Enceladus, backlit by the Sun. Illustrates how far the geysers reach.
Source: NASA

The presence of liquid water and other compounds have led many to speculate/wonder if Enceladus is capable of sustaining some form of life in its ocean. Programs such as the Breakthrough Initiatives and other proposed missions such as the Enceladus Life Finder seek to find whether life does exist somewhere on Enceladus.

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