Comet Holmes is Fading Away

2007-1127holmes.thumbnail.jpg

For a little while there, Comet 17P/Holmes was the largest object in the Solar System, flaring up by a factor of over a million. Its cloud of gas and dust expanded outward to cover a diameter of 1.4 million km (870,000 miles) – bigger than the Sun. Well, the party’s over. Comet Holmes is fading away again. But will it follow history and flare up again?

This image of Comet Holmes was captured by the MMT observatory on November 4th, 2007 using an instrument called “Megacam”. This is one of the largest CCD cameras on Earth, putting 36 9-megapixel CCD chips together to form a single array with 300 megapixels.

The camera captured images of the comet with three separate exposures in three colours to produce this full colour image.

If you want to see Holmes before it fades into obscurity again, you’re going to need binoculars. Although it’s still a 3rd magnitude object, and should be visible with the unaided eye, it’s so large in the sky that it’s actually quite faint now.

Astronomers are hoping that it’ll repeat history. During its last outburst back in 1892, the comet underwent a second bright flareup five months after the first one. So, if history is any judge, we might just see the comet brighten again, and we’ll all get another chance to see it before it’s gone for good.

Original Source: CfA News Release

How Old is Triton’s Surface?

2007-1127triton.thumbnail.jpg

With all of the press going to the moons of Jupiter and Saturn, it’s about time that Neptune got a turn. Triton, one of the moons of Neptune, is curious, with large swaths of the planet resembling the skin of a cantaloupe and a retrograde orbit (opposite that of Neptune’s rotation). Its surface is thought to be rather young, and a new method of counting the craters that pock the moon may push the age of Triton’s surface back even younger than previously thought.

Dr. Paul Schenk of the Lunar and Planetary Institute in Houston, and Kevin Zahnle of the NASA Ames Research Center in California revisited the pictures of Triton’s surface that the Voyager 2 spacecraft took in 1989. By clarifying the images with current technology, they were able to count with very high accuracy the amount of craters, and determine the possible causes of the craters. Their results were published in the July 2007 issue of the journal Icarus, in a paper titled On the negligible age of the surface of Triton.

“Our new crater counts benefit from several improvements in the quality of the Voyager images. Although this does not make invisible craters visible, it does increase the ability to discriminate impact features on Triton,” the researchers wrote.

The images showed that the leading hemisphere — the hemisphere of the planet in the direction of its orbit around Neptune — contains many more craters than that of the trailing hemisphere. Triton is tidally locked to Neptune, which means that – like our Moon – an observer on Neptune would always see the same face of Triton. Thus, the same hemisphere would always face the direction of Triton’s orbit around Neptune.

The researchers propose, “Our map of craters on Triton indicates that all definitive impact craters are on the leading hemisphere. The apparent cratering asymmetry of Triton is extreme. The absence of craters on the trailing hemisphere, and the low frequency of craters near the boundary between leading and trailing hemispheres is unique in the Solar System.”

Since Triton is rotating in the opposite direction of everything else that goes around Neptune, it acts like a giant “vacuum cleaner,” and picks up any debris orbiting the planet in a prograde (the same as Neptune’s rotation) direction.

Triton is thought to have given itself a makeover very recently because it was captured by Neptune long ago; most likely, Triton was one body in a binary system, and when Neptune captured it, the other body was thrown out of the Solar System. After being captured, all of the energy that went into slowing Triton down into orbit around Neptune was transferred into heat that melted the surface and interior of the planet. This heat could have lasted for millions of years, and the tidal energy from Neptune may still warm the interior of Triton today.

Normally, areas that have less craters have been resurfaced more recently, and thus are generally younger than surfaces with lots of craters. By analyzing the density of the craters, and using information about the type and frequency of debris that possibly caused them, the researchers were able to calculate that the terrain on the trailing hemisphere with less craters than that of the leading hemisphere was actually older than the area with more craters.

“Whatever their origin, the paucity of impact craters (and heliocentric craters in particular) suggests that Triton’s surface is very young, younger than 100 million years and possibly as young as a few million years. A return to Neptune and its vigorous, dynamic moon Triton is long overdue,” the researchers wrote.

Source: Icarus

Astrosphere for November 27th, 2007

2007-1127bender.thumbnail.jpg

First, let me direct your attention to the 30th Carnival of Space, hosted by Bad Astronomy. I don’t want to sound like a broken record here, but the Carnival is a great way to increase exposure to your website or blog. If you want more readers, join the carnival.

My absolute favourite television show, Futurama, has a new DVD coming out called Bender’s Big Score. If you like the show, give it some support and buy a DVD. You can find out more here from the official website.

Centauri Dreams talks about the past and future of solar sail technology.

Astronomy Picture of the Day has this image of the International Space Station over the Ionian Sea. Just think what it took to capture that image.

Colony Worlds reports on a new technology that could give solar energy the ability to keep on providing power, right through the night.

Astroprof offers you an easy way to find Mars; just look for the Moon. The two objects are close together right now, and easy to find.

Pamela Gay debunks the recent news that observing the Universe will hasten its demise.

Podcast: Pluto and the Icy Outer Solar System

2007-1126pluto.thumbnail.jpg

It’s been a long journey, 64 episodes, but now we’re back where we began: Pluto. Last time we talked about how Pluto lost its planethood status, so we won’t go over all that again. This time we’re going to talk about Pluto, its moons, the Kuiper belt, and the other icy objects that inhabit the outer Solar System.
Click here to download the episode

Pluto and the Icy Outer Solar System – Show notes and transcript

Or subscribe to: astronomycast.com/podcast.xml with your podcatching software.

Go here if you’d like some Pluto pictures.

What’s Up this Week: November 26 – December 2, 2007

2007-1126ngc457.thumbnail.jpg

Monday, November 26 – Today in 1965 marked the launch of the first French satellite – Asterix 1. Today is also the seventh anniversary of the discovery of the meteorites SAU 005 & 008: the “Mars Meteorites.” These meteorites are known to be of Martian origin because of gases preserved in the glassy material of their interior. They were hurled into space some 600,000 years ago when a probable asteroid impact on Mars tossed them high enough to escape the planet’s gravity, and they were captured by our gravity these many thousands of years later. They are just two of the 32 meteorites found on Earth which have been positively determined from their chemical compositions to be of Martian origin.

Thanks to just a slightly later rise of the Moon, let’s return again to Cassiopeia and start at the central-most bright star, Gamma. Four degrees southeast is our marker for this starhop, Phi Cassiopeiae. By aiming binoculars or telescopes at this star, it is very easy to locate an interesting open cluster, NGC 457, because they will be in the same field of view.

This bright and splendid galactic cluster has received a variety of names over the years because of its uncanny resemblance to a figure. Some call it an “Angel,” others see it as the “Zuni Thunderbird;” I’ve heard it called the “Owl” and the “Dragonfly,” but perhaps my favorite is the “E.T. Cluster,” As you view it, you can see why! Bright Phi and HD 7902 appear like “eyes” in the dark and the dozens of stars that make up the “body” appear like outstretched “arms” or “wings.” (For E.T. fans? Check out the red “heart” in the center.)

All this is very fanciful, but what is NGC 457, really? Both Phi and HD 7902 may not be true members of the cluster. If 5th magnitude Phi were actually part of this grouping, it would have to have a distance of approximately 9300 light-years, making it the most luminous star in the sky, far outshining even Rigel! To get a rough of idea of what that means, if we were to view our own Sun from this far away, it would be no more than magnitude 17.5. The fainter members of NGC 457 comprise a relatively young star cluster that spans about 30 light-years. Most of the stars are only about 10 million years old, yet there is an 8.6 magnitude red supergiant in the center. No matter what you call it, NGC 457 is an entertaining and bright cluster that you will find yourself returning to again and again. Enjoy!

Tuesday, November 27 – Tonight let’s take advantage of early dark and venture further into Cassiopeia. Returning to Gamma, we will move towards the southeast and identify Delta. Also known as Ruchbah, this long-term and very slight variable star is about 45 light-years away, but we are going to use it as our marker as we head just one degree northeast and discover M103.

As the last object in the original Messier catalog, M103 (NGC 581) was actually credited to MÈchain in 1781. Easily spotted in binoculars and small scopes, this rich open cluster is around magnitude 7, making it a prime study object. At about 8000 light-years away and spanning approximately 15 light-years, M103 offers up superb views in a variety of magnitudes and colors, with a notable red in the south and a pleasing yellow and blue double to the northwest.

Viewers with telescopes and larger binoculars are encouraged to move about a degree and half east of M103 to view a small and challenging chain of open clusters, NGCs 654, 663 and 659! Surprisingly larger than M103, NGC 663 is a lovely fan-shaped concentration of stars with about 15 or so members that resolve easily to smaller aperture. For the telescope, head north for NGC 654, (difficult, but not impossible to even a 114mm scope) which has a bright star on its southern border. South of NGC 663 is NGC 659 which is definitely a challenge for small scopes, but its presence will be revealed just northeast of two conspicuous stars in the field of view.

If you are out when the Moon rises tonight, enjoy seeing Mars very nearby – less than 2 degrees away! And speaking of degrees, today is also the birthday of Anders Celsius – born in 1701.

Wednesday, November 28 – Once again utilizing early darkness, let’s go back to Cassiopeia. Remembering Alpha’s position as the westernmost star, go there with your finderscope or binoculars and locate bright Sigma and Rho (each has a dimmer companion). They will appear to the southwest of Alpha. It is between these two stars that you will find NGC 7789 (RA 23 57 24.00 Dec +56 42 30.0).

Absolutely one of the finest of rich galactic opens bordering on a loose globular, NGC 7789 has a population of about 1000 stars and spans a mind-boggling 40 light-years. At well over a billion years old, the stars in this 5000 light-year distant galactic cluster have already evolved into red-giants or super-giants. Discovered by Caroline Herschel in the 18th century, this huge cloud of stars has an average magnitude of 10, making it a great large binocular object, a superb small telescope target, and a total fantasy of resolution for larger instruments.

Tonight in 1659, Christian Huygens was busy at the eyepiece – but he wasn’t studying Saturn. This was the first time any astronomer had seen dark markings on Mars!

Thursday, November 29 – Today in 1961, Mercury 5 launched Enos the Chimp into fame!

With a short time until the Moon rises tonight, why not journey with me once again to Cassiopeia? We will start our studies with the western-most of the bright stars – Beta. Also known as “Caph,” Beta Cassiopeiae is approximately 45 light-years away and is known to be a rapid variable. Viewers with larger telescopes are challenged to find the 14th magnitude optical companion to Caph at about 23″ in separation. Tonight, using our previous study stars Alpha and Beta, we are going to learn to locate a Messier object with ease! By drawing an imaginary line between Alpha and Beta, we extend that line the same distance and angle beyond Beta and find M52.

Found on September 7, 1774 by Charles Messier, this magnitude 7 galactic cluster is easily seen in both binoculars and small telescopes. Comprised of roughly 200 members, this open cluster is roughly 3,000 light-years distant and spans approximately 10-15 light-years. Containing stars of several different magnitudes, larger telescopes will easily perceive blue components as well as orange and yellow. Also known as NGC 7654, M52 is a young, very compressed cluster whose approximate age is about the same as the Pleiades.

For those with large telescopes wanting a challenge? Try spotting a faint patch of nebulosity just 36′ to the southwest. This is NGC 7635, more commonly known as the “Bubble Nebula.” Best of luck!

Friday, November 30 – If you are up before dawn, Look for bright Venus and cool, blue Spica less than a fistwidth apart – and look for the Moon and Regulus! Less than half a degree of separation means a possible occultation event, so be sure to check IOTA information. Just as a curiosity, on this day in 1954, Elizabeth Hodges was struck by a five kilogram meteorite in Alabama. Duck!

Tonight we will haunt Cassiopeia one last time – with studies for the seasoned observer. Our first challenge of the evening will be to return to Gamma where we will locate two patches of nebulosity in the same field of view. IC 59 and IC 63 are challenging because of the bright influence of the star, but by moving the star to the edge of the field of view you may be able to locate these two splendid small nebulae. If you do not have success with this pair, why not move on to Alpha? About one and a half degrees due east, you will find a small collection of finderscope stars that mark the area of NGC 281 (RA 00 52 25.10 Dec +56 33 54.0). This distinctive cloud of stars and ghostly nebulae make this NGC object a fine challenge!

The last things we will study are two small elliptical galaxies that are achievable in mid-sized scopes. Locate Omicron Cassiopeiae about 7 degrees north of M31 and discover a close galactic pair that is associated with the Andromeda group – NGC 185 (RA 00 38 57.40 Dec +48 20 14.4) and NGC 147 (RA 00 33 11.79 Dec +48 30 24.8).

The constellation of Cassiopeia contains many, many more fine star clusters, and nebulae – and even more galaxies. For the casual observer, simply tracing over the rich star fields with binoculars is a true pleasure, for there are many bright asterisms best enjoyed at low power. Scopists will return to “rock with the Queen” year after year for its many challenging treasures. Enjoy it tonight!

Saturday, December 1 – Born today in 1811 was Benjamin (Don Benito) Wilson. He was the namesake of Mt. Wilson, California – home to what once were the largest telescopes in the world – the 60″ Hale and the 100″ Hooker. Later, three solar telescopes were added on the mountain – two of which are still in use – as well as the CHARA array and active interferometers. It was here that Edwin Hubble first realized the “nebulae” were distant galaxies and discovered Cepheid variables in them. As we approach the end of our SkyWatching year together, let us pretend the skies are still as dark as they were on Mt. Wilson as we aim our binoculars and telescopes towards one of the most elusive galaxies of all – M33.

Located about one-third the distance between Alpha Triangulum and Beta Andromedae (RA 01 33.9 Dec +30 39), this member of our Local Group was probably first seen by Hodierna, but was recovered independently by Messier some 110 years later. Right on the edge of visibility unaided, M33 spans about 4 full moon widths of sky, making it a beautiful binocular object and a prime view in a low power telescope.

Smaller than the Milky Way and the Andromeda Galaxy, the Triangulum galaxy is about average in size, but anything but average to study. So impressed was Herschel that he gave it its own designation of H V.17 after having cataloged one of its bright star forming regions as H III.150! In 1926, Hubble also studied M33 at Mt. Wilson with the Hooker telescope during his work with Cepheid variables. Larger telescopes often “can’t see” M33 with good reason – it overfills the field of view – but what a view! Not only did Herschel discover a region much like our own Orion Nebula, but the entire galaxy contains many NGC and IC objects (even globular clusters) that can be seen with a larger scope.

Although M33 might be 3 million light-years away, tonight it’s as close as your own dark sky site…

Sunday, December 2 – If you are awake before dawn, enjoy the beauty of Saturn and the Moon as they dance along the ecliptic plane together. For most viewers, the tranquil pair will only be about a fingerwidth apart. Today in 1934, the largest mirror in telescope history began its life as the blank for the 200″ telescope was cast in Corning, NY.

The 200″ would play another important role as Edwin Hubble continued on at Palomar Observatory. Thanks to his work there, we now understand “Hubble’s Law” – the expansion of the Universe. Tonight let us honor that great mind as we take a look at a galaxy that’s receding from us – NGC 1300.

Located about a thumb’s width north of Tau4 Eridani (RA 03 19.7 Dec -19 25), this is probably the most incredible barred spiral you will ever encounter. At magnitude 10, it will require at least a 4.5″ telescope in northern latitudes, but can probably be spotted with binoculars in the far south.

At 75 million light-years away, NGC 1300’s central bar alone is larger than the Milky Way, and this galaxy has been intensively studied because the manner of its formation was so similar that of to our own. Although it is so distant, it is seen face-on – allowing us a look at how this formation occurs without looking through the gas and dust which block our own central view. Enjoy this one’s fantastic structure!

Could Antimatter Be Powering Super-Luminous Supernovae?

2007-1126supernova.thumbnail.jpg

Explosions are almost always cool, and supernovae are some of the most spectacular and violent explosions in the Universe. In 2006, the supernova SN 2006gy wowed scientists with a light show that was 10 times as luminous as the average supernova, challenging the traditional model of exactly how an exploding star creates a supernova. Astronomers suspect that the cause is the repeated production of antimatter in the core of the star.

Supernovae occur when a star nears the end of its life, and the nuclear processes that fuel the star push outward more powerfully than the force of gravity can hold the star together; the type of supernova created depends on the mass of the star. In stars with masses between 95-130 times the Sun, this process can occur more than once, creating a “pulsational” supernova which can happen as many as seven times.

The cause for the multiple explosions may have to do with the production of antimatter particles in the core, which then recombine and release large amounts of energy.

“The pair instability is encountered when, late in the star’s life, a large amount of thermal energy goes into making the masses of an increasing abundance of electron-positron pairs rather than providing pressure,” wrote Dr. Stan Woosley, of the Department of Astronomy and Astrophysics, USCS Santa Cruz.

What happens is this: the first supernova occurs, powered by the antimatter explosions in the core, and ejects a large amount of the star’s material out into space; however, there still remains enough matter near the core for the star to reignite and begin nuclear processes once again. After between a few hundred days and a few years, another supernova occurs by the same mechanism, and when the ejected material collides with the previous shell of ejected material, the interaction gives off enormous amounts of light.

This process only occurs with stars in the 95-130 solar mass range. Stars with solar masses under 95 undergo typical, non-repeating supernovae, while those over 130 solar masses are subject to the pair instability but explode with such force as to leave nothing near the core to recombine and start the process again.

The production of antimatter in the core, as well as the large amount of light given off by the repeated collision of the shells of ejected matter explains very well the otherwise puzzling luminosity of SN 2006gy.

“The model existed before 2006gy happened as well as the prediction of a possible bright supernova of this sort. When we learned of the supernova, we carried out much more detailed calculations specific to 2006gy and found, to our satisfaction, that many of the observed facts were in the model results,” Dr. Woosley said.

There are other possible candidates for this type of repeating supernova, including Eta Carinae, though they unfortunately may not all be as spectacular as SN 2006gy.

Source: Arxiv paper

Pure Carbon Stars Discovered

2007-1126dwarf.thumbnail.jpg

When stars like our Sun run out of fuel, they die a long slow death as a white dwarf, slowing cooling down over billions of years. But now an international team of astronomers has found an unusual form of white dwarf with a bare carbon core; one that might suggest a new sequence of stellar evolution. A fate for stars right on the edge of detonating as supernovae.

The majority of stars that die eventually become white dwarfs in the end. The most massive 2-3% of stars will actually detonate as supernovae when they end their lives. But these newly discovered objects might have been right at the borderline. If they were just a little more massive, they would have detonated as well, but instead, they didn’t quite make it.

The evidence was gathered by astronomers from the University of Arizona, Université de Montréal and Paris Observatory. They reviewed more than 10,000 new white dwarfs found in the most recent update to the Sloan Digital Sky Survey. This automated survey has turned up four times as many white dwarf stars as previously known.

As stars run out of hydrogen, they switch to helium, and as this burns off, they’re left with a core of carbon and oxygen surrounded by an atmosphere of hydrogen or helium. That’s what a normal white dwarf looks like.

But a small group of these white dwarfs have a very bizarre appearance. They’re just a bare core of carbon, without any surrounding atmosphere of hydrogen or helium.

From the press release announcing the discovery, researcher Patrick Dufour describes the discovery, “when I first started modeling the atmospheres of these hotter DQ stars, my first thought was that these are helium-rich stars with traces of carbon, just like the cooler ones. But as I started analyzing the stars with the higher temperature model, I realized that even if I increased the carbon abundance, the model still didn’t agree with the SDSS data. Out of pure desperation, I decided to try modeling a pure-carbon atmosphere. It worked. I found that if I calculated a pure carbon atmosphere model, it reproduces the spectra exactly as observed. No one had calculated a pure carbon atmosphere model before. No one believed that it existed. We were surprised and excited.”

The researchers believe you need to have a star with 9-11 solar masses to create a carbon star like this. They’re planning follow up observations to better pinpoint the masses of the objects they’ve discovered so far.

Original Source: UA News Release

Inflatable Lunar Habitat to Be Tested in Antarctica

2007-1123habitat.thumbnail.jpg

As humans prepare to return to the Moon, this time to stay, there are so many different technologies that need to be developed and tested. NASA and the NSF are testing out a new prototype for an inflatable habitat that might eventually protect humans on the Moon. And they’re testing it in the most extreme place on Earth: Antarctica.

The newly developed inflatable habitat is inflated and pressurized, giving potential astronauts their own atmosphere. Inside the tent is heated, offering up 35 square metres (384 square feet) of living space, under a 2.4-metre (8-foot) ceiling. It also has access points for electrical power.

NASA currently uses a 50-year old tent design called a Jamesway hut. Television viewers will recognize these designs in the show M*A*S*H. Although there are new approaches to this old design, they’re rigid, difficult to ship, and have limited insulation. When you’re working in Antarctica, a lack of insulation is a serious problem.

The purpose of this new design is to test out how well an inflatable habitat will work in terms of packing, transportation, set up, power consumption and damage tolerance.

When astronauts do finally return to the Moon by 2020, they’ll be setting up a permanent lunar outpost. An inflatable habitat like this could be carried on future lunar rovers, and would allow the astronauts to set up a temporary home, far away from the permanent base. This would greatly increase their range, and allow the exploration of the most interesting lunar features – not just those nearby the base.

The inflatable habitat is being developed under NASA’s Innovative Partnerships Program.

Original Source: NSF News Release

Meteorites Reveal Mars’ Past: Molten Surface, Thick Atmosphere

hst_mars_opp_9709a.thumbnail.jpg

If Mars ever had water flowing on its surface, as the many canyons and riverbed-like features on the Red Planet seem to indicate, it also would have needed a thicker atmosphere than what encircles that planet today. New research has revealed that Mars did indeed have a thick atmosphere for about 100 million years after the planet was formed. But the only thing flowing on Mars’ surface at that time was an ocean of molten rock.

A study of Martian meteorites found on Earth shows that Mars had a magma ocean for millions of years, which is surprisingly long, according to Qing-Zhu Yin, assistant professor of geology at the University of California- Davis. For such a persistent event, a thick atmosphere had to blanket Mars to allow the planet to cool slowly.

Meteorites called shergottites were studied to document volcanic activities on Mars between 470 million and 165 million years ago. These rocks were later thrown out of Mars’ gravity field by asteroid impacts and delivered to Earth — a free “sample return mission” as the scientists called it — accomplished by nature.

By precisely measuring the ratios of different isotopes of neodymium and samarium, the researchers could measure the age of the meteorites, and then use them to work out what the crust of Mars was like billions of years before that. Previous estimates for how long the surface remained molten ranged from thousands of years to several hundred million years.

The research was conducted by the Lunar and Planetary Institute, UC Davis and the Johnson Space Center.

Planets form by dust and rocks coming together to form planetisimals, and then these small planets collide together to form larger planets. The giant collisions in this final phase would release huge amounts of energy with nowhere to go except back into the new planet. The rock would turn to molten magma and heavy metals would sink to the core of the planet, releasing additional energy. The molten mantle eventually cools to form a solid crust on the surface.

Although Mars appears to no longer be volcanically active, NASA’s Mars Global Surveyor Spacecraft discovered that the Red Planet hasn’t completely cooled since its formation 4.5 billion years ago. Data from MGS in 2003 indicated that Mars’ core is made either of entirely liquid iron, or it has a solid iron center surrounded by molten iron.

Original News Source: UC Davis Press Release

Seeing Inside the Earth with Neutrinos

2007-1121icecube.thumbnail.jpg

You know what it’s like to get an X-ray done: you go to the doctor, get in a large machine, she puts on a lead vest, and X-rays shoot through your body, forming a picture of your skeletal structure. Well, using the IceCube neutrino detector – as well as other neutrino detectors to come – it might be possible to do something very similar to this, but to the Earth.

A collaborative team of physicists and geologists from around the world has proposed that with the construction of IceCube, a neutrino detector at the South Pole, it should be possible to get a very accurate picture of the Earth’s core using neutrinos that stream through the Earth from the other side. Their recent paper is entitled Imaging the Internal Structure of the Earth with Atmospheric Neutrinos.

Neutrinos are particles with very small mass that don’t interact with other types of matter very often. There are trillions of them streaming through your body this very second, but don’t worry: the chance that they will interact with any of the protons or neutrons that make up your body are very, very low. The higher the energy of the neutrino, the more likely it is to interact with a particle that has mass. When this happens a cascade of other particles is created, and a particle called a muon that is produced by this reaction can be detected.

Neutrino telescopes don’t look anything like your average viewing telescopes; rather, they are made up of a huge block of matter, usually water or ice. IceCube is just such a detector, made up of one cubic km of ice at the South Pole. There are small “strings” of detectors placed strategically in the ice to record the presence of muons from neutrino-particle interactions. The large mass of the detector increases the likelihood of finding the collisions between neutrinos and other particles.

The idea to use neutrinos as a way to image Earth’s interior has been around for more than 25 years, but IceCube is the first neutrino telescope with the ability to detect neutrinos at the energies necessary to give an accurate picture of the core.

Using IceCube to view the inside the Earth would increase our understanding of the “core-mantle transition” – where the Earth’s core meets the mantle – because this method is more accurate than methods currently used to estimate what the inside of the Earth looks like.

Dr. Francis Halzen of the University of Wisconsin Department of Physics, one of the co-authors of the research paper proposes, “we can see the transition “directly” and not infer it from some analysis of indirect data, such as data on Earth sound waves. The precision of our mapping is directly related to our angular resolution on the path taken through the Earth by a neutrino.”

Much like in an X-ray, some of the neutrinos coming through the Earth would be blocked by the dense core – like the Earth’s “skeleton” – while those streaming through the mantle, which is less dense, would be detected by IceCube.
Though the IceCube telescope is still under construction, it has already begun taking data, and will only continue to improve as more detectors are added to the ice.

Dr. Halzen said, “An unusual feature of IceCube is that we operate the partially deployed detector while we are constructing it. We have been collecting data relevant to this problem for more than 1 year and hope to run half the detector starting this February, i.e. after another construction season over the Antarctic summer that just started.”

The imaging is expected to be finished anywhere between the next 3 and 10 years.

Source: Arxiv Paper