Some Planets Are Just So Extra… (Extrasolar, That Is)

An extrasolar planet, or an exoplanet, is one which orbits a star other than our Sun. These planets provide interest and opportunities for research, because under the correct conditions, such as those upon Earth, there is a possibility that life could exist and/or be discovered upon these planets.

By observing exoplanets, and specifically searching various factors and elements present upon the planet, it can by hypothesized whether or not the planet could potentially support some form of life. One thing that is sought after during examinations of these planets, is the presence of water, as that would be necessary to support life forms similar to our own. The Spitzer Space Telescope examines exoplanets, in order to search for things such as water.

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Photo Credit: NASA/JPL-Caltech/T. Pyle (SSC)

The above rendering (artistic rendering) depicts a dry planet, such as those observed in the HD 209458b and HD 189733b star systems that Spitzer has observed to determine if water is present. The planets in question are called “hot Jupiters”, which are the similar in size to Jupiter, but are closer to their star, like Earth compared to our own Jupiter. The planets were examined for water by checking the infrared outputs of the stars before and after eclipse to determine the atmospheric conditions upon the planets. While the planets checked in those star systems did not have water, the fact that it is possible to check for it is a significant advancement in terms of exoplanets.

Clearly, distance from the star is an important factor in the conditions of exoplanets, as is the output of the sun in question, and the planet Gliese 1214b demonstrates this concept quite well. Gliese 1214b orbits Gliese 1214, a star smaller and cooler than our own Sun, however the planet also orbits much closer to its star than Earth does. The artist rendering below depicts the planet and its star.

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Photo Credit: ESO, L. Calçada

The other significant difference that factors into the conditions of Gliese 1214b is the size of the planet. It has been denoted as a “super-Earth”, because the planet is slightly larger than Earth, but not as large as planets such as Neptune. It has been proposed that the surface would be too hot to support the existence of liquid water, however it is possible that water in the form of steam may be present upon the planet.

Sources: 1, 2


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Blog 4: Electron Rainfall

Picture

 

Earths two radiation belt known as the Van Allen belts where discover in 1958. But recent discoveries have shown that a third belt will sometimes appear. The image above shows the three belts in yellow and green represents the space between them.

The Van Allen Belts since they are regions of dynamic radiation are regions high-energy particles; they are trapped there by the earth’s magnetic field. These particles can gain and lose energize particles. they gain the particles from radiation from the sun. But they lose of particles is more interesting and can be depleted by a thousand-fold in mere hours. The loss of particles happens when intense bouts of solar radiation disturbs the earth’s magnetic field, causing drop-outs which are times when the belts lose a dramatic number of particles. Drop-outs involve power electromagnetic waves which scatter ultra-relativistic electrons in the radiation belt. This means the electrons will move down the waves and go into the atmosphere, or rain into the atmosphere. This occurs in the lower region of the belts close to earth.

Sources:

Radiation Belt and Electron Rainfall


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Blog 4 – The Sunspot Cycle and Earth’s Climate

For this blog I thought I’d write about how sunspots affect the Earth’s climate, as I am studying environmental sciences and I recently took Professor Gilligan’s Global Climate Change course (highly recommended and it counts for AXLE).  Sunspots are the most interesting feature on the sun’s surface.  They are the dark patches that periodically appear on the surface of the sun.  They appear dark not because they really are black, but because they are much cooler than the plasma around them.  Sunspots average 4000 K while the rest of the sun’s surface averages 5800 K.  There is a cycle to sunspots, alternating between a solar minimum and solar maximum.  The time between maximums averages 11 years, but can range from 7 to 15 years.

Overall, the sun’s total energy output changes very little – maybe by 0.1% at most.  The output of ultraviolet radiation and Xrays can vary more significantly.  There is discussion considering whether solar activity might affect Earth’s climate.  One correlation is that the Maunder minimum, where solar activity appears to have completely ceased during the period 1645-1715, was at the same time as the Little Ice Age, where temperatures in Europe and North America dropped exceptionally low.  Some scientists believe that weather changes, such as periods of drought or more frequent storms, may also be attributed to solar cycles.  Still fewer scientists believe that changes in the Sun may be causing recent global warming, although close to every climate model attributes the blame to humans.  Still, the study of how the Sun may affect our climate remains an active area of research.sunspots_max_min_sm

Solar Maximum/Solar Minimum


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Blog #4: How did the Moon form?

 

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Representation of Giant Impactor Theory

For a long time, we were generally unsure of how Earth’s moon originally formed, and there were a few popular theories which were later disproven. Below are original theories about the formation of the Moon and how they were disproven:

  1. Fission Theory:

This theory is based on the fact that the chemical composition of the Moon is somewhat similar to that of Earth’s mantle. The theory proposes that in the early days of the solar system, the Earth was spinning so quickly that a piece of it was flung off of one of its outer layers, and eventually went into orbit around the Earth. This theory does not hold up because there is no “fossil evidence” of the rapid spinning at the basis of this theory.

  1. Capture Theory:

This theory suggests that the Moon was a particular object flying through space that got captured by the Earth’s gravitational field, thus sending the Moon into orbit around the Earth. This theory does not hold up given the likelihood that the Moon was formed in some way from the Earth (similar chemical composition) and because it is unlikely that the Moon slowed down enough to become captured by Earth’s gravitational field.

  1. Condensation Theory:

This theory suggests that the Earth and Moon were formed individually and at the same time, from the nebula that formed the solar system. This seems to make sense given that the Earth and the Moon have similar composition, however, they would have to have a far more similar composition for this to be possible (the Moon should have an iron core, but it does not).

 

The theory which is widely accepted today is called the Giant Impactor Theory, and suggests that the Moon was formed through a collision between the newly formed Earth and a rock about the size of Mars. Astrophysicist Mastrobuono-Battisti simulated collisions in the early solar system and found that most simulations produced 3 to 4 rocky planets comparable to Earth. Around 30% of the time, the composition of one planet was very similar to that of the last planet that collided with it, providing additional evidence in favor of the Giant Impactor Theory.

 

Sources:

How the Moon Formed: Violent Cosmic Crash Theory Gets Double Boost

StarChild Question of the Month for October 2001


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Blog #6

250px-ceres_-_rc3_-_haulani_crater_282238113169129_28cropped29Image of Ceres

The asteroid belt lies between Mars and Jupiter. This area is where the dwarf planet Ceres is located. Given that it was the first dwarf planet to be visited by a spacecraft and the largest object in the asteroid belt, there have been quite a few interesting discoveries about this celestial object. Here are a few:

  1. Ceres actually makes up ¼ of the asteroid belt’s mass.
  2. Ceres is about the same size as the state of Texas!
  3. Like Pluto, Ceres has actually gone through many different categorizations. It started out as a comet, was later deemed a planet, was later labelled an asteroid, and then finally was called a dwarf planet in 2006 (the same year Pluto got demoted)!
  4. The name for this dwarf planet comes from the Roman goddess of harvests.
  5. It was first sighted by Giuseppe Piazzi in 1801. 
  6. Recent research has demonstrated that the gravity from some of the gas giants (like Saturn and Jupiter) may actually influence Ceres’ orientation. A new study based on NASA’s Dawn mission showed that there have been quite dramatic (in terms of astronomical time!) variations in the axial tilt of Ceres over a course of 24,500 years. This is important because when axial tilt is small, there are some large areas on Ceres that don’t get any kind of direct light from the sun. These “permanently shadowed regions” could possibly have a low enough temperature to allow for frozen water (ice) on the surface of the dwarf planet.

Hope you learned a little more about Ceres!

Sources: Ceres General InformationIce Linked to Tilt History


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Juno Probe Makes Fourth Passage of Jupiter’s Clouds

 

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©2017 NASA/JPL-Caltech

Last Monday (March 27), NASA’s Juno spacecraft made a historic passage within the vicinity of the cloud tops of Jupiter’s atmosphere, marking its fifth overall flyby of the gas giant and fourth “science pass”, or experimental run. The probe marked its closest point to the planet at 08:52 GMT, coming within 2700 miles of its cloud tops as it collected information on the planet’s atmospheric makeup, mostly consisting of molecular hydrogen and helium, as well as traces of compounds such as water, hydrogen sulfide, or phosphine to name a few.

The probe has been orbiting Jupiter since summer of 2016, coming within its closest distance of the planet every 53 days or so. A modified plan to enter a closer orbit that would have decreased the orbital time to 14 days instead was originally pitched to increase the number of close encounters, however it was immediately put to rest after issues with the space probe’s helium valves.

For more on the Juno spacecraft and a video explaining its path and purpose, click here.


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Blog #5

new_horizons_mission_mission_path_overviewAn Overview of the New Horizons Mission

The Kuiper Belt is a very fascinating region of our solar system consisting largely of icy bodies and comets. Thus, there is a lot of really interesting research aiming to better understand the Belt itself and the objects that call it home. One NASA initiative in this regard is the New Horizons spacecraft. This spacecraft, which was launched on January 19th, 2006, made history in July of 2015 when it reached Pluto. The aim of New Horizons was to study Kuiper Belt objects and it held particular concern for Pluto and its moons. Since 2014, New Horizons has made many observations about Kuiper Belt objects and has collected data about the dust and particle environment that makes up this region of space. It has also studied the heliosphere. If it continues along the path that it has, New Horizons is predicted to fly past MU69 (another Kuiper Belt object) on January 1st, 2019.  This flyby would set a new record for the farthest world explored in the history of human civilization.

To get you a little excited about this event here are some facts about the Kuiper Belt:

  1. The Kuiper Belt was named after Gerard Kuiper, an astronomer who first predicted the existence of this region of space. It took another 18 years for scientists to find the proof to support this prediction.
  2. The Kuiper Belt extends from about 30 to 55 AU.
  3. The comets in the Kuiper Belt take less than 200 years to fully orbit the sun. On the other hand, long-period comets originate from the Oort Cloud and take longer than 200 years to complete their orbit around the sun.

Sources: New HorizonsInformation about New Horizon flyby dates


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SpaceX Makes History

On March 30th, 2017, SpaceX made history by successfully launching and landing a used rocket. The company created by Elon Musk used the Falcon 9 to to send a satellite into space and then landed in on a ship in the Atlantic Ocean. This rocket was initially launched in April of 2016, and the launch this March marks its second mission. The actual part of the rocket that was reused was the booster, which is the most expensive part of the rocket.

This incredible milestone in the history of space travel shows lots of promise for commercial space travel. Typically, rockets can cost millions and millions of dollars, but the hope of reusing rockets is changing the game. Elon Musk says “It’s the difference between having airplanes that you threw away after every flight, verses reusing them multiple times”. This is a huge breakthrough for Musk and the field of space travel in general. Elon Musk, what’s next?

Source: Recode


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X-Ray Burst Baffles Scientists

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Image of the burst known as CDF-S XT1 with time lapse images of the event below

In 2014, NASA’s Chandra X-ray Observatory spotted a large, sudden flash, producing the deepest x-ray image ever. Today, this flash still baffles scientists who are attempting to understand its origin. It was given the name CDF-S XT1 and was spotted in an area of the sky known as the Chandra Deep Field South. When the event happened, a previously dark spot in the sky became 1000 times brighter within just a few hours. This burst faded back to its original darkness within just a day.

Scientists can only speculate what caused this enormous burst because none of their current models match up with the data from this event. However, they do have some guesses as to what happened. There are three main hypotheses. The first two involve gamma ray bursts, caused either by the collision of two neutron stars or the collapse of a star. The third hypothesis is that a black hole consumed a white dwarf star. The other idea is that they witnessed a totally new cataclysmic event that had never been witnessed before. The scientists continue to comb over archives of data to find events with similar properties to the burst of CDF-S XT1. Perhaps the origin of the event will remain unknown until more bursts like this are spotted.

 

 

Sources:

space.com


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Blog #4

Robert Lightfoot gets a tour of the SAGE 111 ProgramImage of SAGE III

Climate change is an oft-mentioned topic in a diverse range of conversations including those within the scientific community and increasingly in the political sphere as well. Despite a lot of ongoing talk about climate change, I think that many ordinary citizens, including myself, don’t have a good grasp of the science and math that explains climate change-or how it is measured. In this post, I am going to discuss some of the instruments that NASA and other space agencies use to actually help monitor the health of our own planet’s climate. SAGE (Stratospheric Aerosol and Gas Experiment) I and SAGE II are two instruments that were mounted to satellites that aimed to understand the origins and consequences of the Antarctic ozone hole. In 1987, the Montreal Protocol banned gases that could destroy ozone. The aim of this measure was to recover the ozone layer, which protects the Earth from the sun’s UV radiation. In order to monitor this recovery process, SAGE III was launched to the International Space Station on the SpaceX Dragon capsule in February of this year. SAGE III is expected to remain in use for at least three years. In the past, other instruments have also been launched to help measure and understand climate change.  For instance, in 2015, the Cloud Aerosol Transport System was attached to the ISS for the purpose of collected data that can be used in air quality research and climate modelling.

Source:NASA Measuring Climate Change


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