The Strange Case of Supernova SN2008ha

Image of SN2008ha in the galaxy UGC 12682 in Pegasus.

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Almost immediately after it was discovered last November by 14-year-old Caroline Moore of the Puckett Observatory Supernova Search Team, professional astronomers knew supernova SN2008ha was a strange one.  The spectra of the blast showed no signs of hydrogen, which meant it must be a Type Ia supernova caused by the explosion of a white dwarf accreting matter in a binary star system.  But if so, why was it some 50 times fainter than other supernova of its type?

Now in a controversial new paper in the journal Nature, astronomers from Queen’s University Belfast have proposed a new explanation of this supernova.  The researchers, led by Dr. Stefano Valenti, suggest that even though the explosion contained no hydrogen, SN2008ha could be a Type II supernova, the kind caused by the core collapse of a massive star.

Valenti and his colleagues argue that, despite the lack of hydrogen, the spectrum of SN2008ha more closely resembles Type II supernovae.  They cite the lack of emission lines from ionized silicon as as evidence of why SN2008ha is not a Type Ia.  And they cite other supernovae that exhibited similar characteristics, which he says might be less extreme examples of hydrogen-deficient Type II supernovae.

“SN2008ha is the most extreme example of a group of supernovae that show similar properties”, said Dr. Valenti. Up until now the community had thought that they were from the explosion of white dwarfs, which we call type  Ia supernovae. But we think SN2008ha doesn’t quite fit this picture and appears physically related to massive stars”.

But if SN2008ha is a Type II supernova, where did the hydrogen go?  The answer might be mass loss.  Some stars are so massive and luminous that they lose their outer hydrogen layers in strong outflowing stellar winds.  And because they’re so massive, their cores collapse into a black hole without transfering energy to the outer layers of the star, which may explain the low luminosity of the explosion.

“The implications are quite important. If this is a massive star explosion, then it is the first one that might fit the theoretical models of massive stars that lose their outer layers through their huge luminosity pressure and then, perhaps, collapse to black holes with a whimper”, said Dr. Valenti.

Professor Stephen Smartt from Queen’s added “This is still quite controversial, we have put this idea forward and it certainly needs to be taken seriously.

Dr. Valenti’s team is keen to use new deep, time resolved surveys of the Universe to find more of these and test their ideas. One such experiment is the first of the Pan-STARRS telescopes that has started surveying the sky in the last month.

Source:  Queen’s University Belfast

Original Paper:  Nature

Beauty and the Beast: The Corona Australis Nebula by Eddie Trimarchi

The Corona Australis Nebula by Eddie Trimarchi

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Embedded in the Southern Crown some 424 light years away from us resides an area of incredible beauty surrounded by a dark and dusty beast. The three nebulae NGC 6726-27, and NGC 6729 were first discovered by Johann Friedrich Julius Schmidt, during his observations at Athens Observatory in 1861… a time when what they were was poorly understood. At first glance, one might believe this association of stars to be purely coincidental – a chance meeting of moving stars passing through a dust cloud, much like the Pleiades. But, thank heavens for an astronomer named Marth who independently recovered it in 1864 and began to study it, because there’s a whole lot more here than just a pretty picture.

When Marth recovered Schmidt’s three nebulous regions from his vantange point in Malta, he began a series of observations that would last for several years and lead to findings that would cause astronomers to take second looks at this incredible region known as the Corona Australis Nebula. Why? Because by 1916 both Schmidt and Marth had identified a variable star (R CrA) and a variable nebula within it. Within months, astronomers also realized also noticed that the behaviour of R CrA (variability and environment) was similar to T Tauri.

Buried in its yellowish cocoon near the two bright reflection nebulae, R CrA is a young star still accreting interstellar material on to its surface. But what materials? “The 3 micrometers absorption due to H2O ice was detected in three types of sources including protostars, T Tauri-like stars, and background field stars.” says Masuo Tanaka (et al), “This scattered distribution suggests the significant contribution of the circumstellar hot dust to the H-K color and/or sublimation of H2O ice at the inner region of the circumstellar disk due to heating by protostars. Among them, the optical depth of CO ice in IRS 2 is the largest so far detected. It is found that the absorption feature of each source has almost the same central frequency and FWHM which coincide with the calculated values of small grains with dominant CO mantle. On the other hand, the column density of CO ice is found to be substantially smaller than that of H2O ice.”

However, when examined in infrared, two distinct red patches can also be seen hiding inside the beast – Herbig Haro objects. Are these what account for the variability of the nebula? “We suggest that these variations are the result of variable obscuration, possibly linked to dust shells physically associated to the system.” says L.P. Vaz (et al), “NGC 6729 is part of a nebulous region that contains both variable stars R CrA and detached Herbig Be eclipsing binary TY Coronae Australis. We present the non-eclipse-related photometric variability of the system.” Regions that are constantly changing, yet show visible signs of star formation occurring deep inside the dark dust clouds… Coughed out from the hidden star-forming beast (often in pairs) and sent flying in an opposite direction.

Just how long ago were these expelled? According to recent research the primary TY CrA star is difficult to pinpoint, but may be around 3.16 million years old zero-age main sequence, and its secondary star is a pre-main-sequence star located at the base of the Hayashi tracks. It simply isn’t very evolved yet and could be as young as 1.64 million years or as old as 3 million. “All genuine Herbig stars in our sample are located between the birthline and the zero-age main sequence (ZAMS) in the Hertzsprung-Russell diagram (HRD), in accordance with what is expected for pre-main sequence stars.” says M.E. van den Ancker (et al), “The region in the HRD close to the birthline is relatively devoid of stars when compared to the region closer to the ZAMS, in agreement with the expected evolutionary time scales. The Herbig Ae/Be stars not associated with star forming regions were found to be located close to the ZAMS.”

But it is the combination of the beauty of new star formation and the beast of the dust that make the Corona Australis Nebula such a wonderful area for study. By studying polarization, we learn so much more about what is hidden inside. For example, dark dust clouds with embedded star clusters have a more complex distribution of polarization direction than do clouds without clusters, and it is believed that young stars and dense gases are a major factor in the enhanced dispersion of polarization angle – not just quantity of stars. Yet we can take an even closer look! “Polarization mapping of the reflection nebula NGC 6729 reveals parallel bands of polarization vectors across the premain sequence stars R and T Cr A. These bands can be explained by dust discs in which the grains are aligned by toroidal magnetic fields. The dust discs are oriented parallel to each other (in projection and possibly in space) in a north-south direction, which is orthogonal to the axis of the CO bipolar outflow from R Cr A observed by Levreault. Optical jets are associated with both stars, two with R Cr A and one with T Cr A, which are either parallel or antiparallel to each other; however, the optical jets are not orthogonal to the planes of the discs, but are inclined at about 60 deg.” says D. Ward-Thompson of Durham University, “A model is suggested in which the optical jets are collimated by a small inner circumstellar disc, which has decoupled from the magnetic field in outer regions because of ambipolar diffusion, and whose orientation is determined principally by the angular momentum. The large outer interstellar disc, in which the grains are aligned by a toroidal magnetic field, is inclined obliquely to the inner disc and is responsible for the collimation of the CO bipolar outflow.”

Is is the dark clouds of the beast hiding the beauty of star formation that causes the variability? “Measurable changes in the surface brightness of the reflection nebula associated with R CrA occur over intervals as short as 24 hours. These and other more extreme variations are demonstrated with CCD images obtained over a 23-day period. During this time span R CrA brightened by 1.3 mag.” says J.A. Graham, “The alterations in the appearance of the nebula NGC 6729 are apparently caused by the shadowing effects of clouds which are very close to the star, probably well within 1 Au. The spectrum of R CrA may itself vary slightly from night to night, and these changes are echoed by the surrounding nebula with an observable time delay.”

Will we ever know everything there is to know about the Beauty and the Beast? What we do know is: “The the Corona Australis molecular cloud complex is one of the nearest regions with ongoing and/or recent star formation. It is a region with highly variable extinction, containing, at its core, the Coronet protostar cluster. There are now 55 known optically detected members, starting at late B spectral types. At the opposite end of the mass spectrum, there are two confirmed brown dwarf members and seven more candidate brown dwarfs. The Corona Australis molecular cloud complex is today known as one of the nearest regions with ongoing and/or recent intermediate- and low-mass star formation.” says Ralph Neuhauser of Astrophysikalisches Institut und Universitats-Sternwarte, “In between the stars R and T CrA, there is the reflection nebula NGC 6729, and the stars TY CrA and HD 176386 illuminate the nebula NGC 6726/6727. Studying lines of CN, CH, and CH in the direction of TY CrA, find that the dust in the region which is attenuating the UV emission is highly processed and strong extended emission is possibly due to polycyclic aromatic hydrocarbons (PAHs).”

Our thanks to Eddie Trimarchi of Southern Galactic for sharing this awesome photo with us!

Watch Press Conferences Live From AAS


Wish you were at the A A S conference in Pasadena, California? You can watch the press conferences today live, via Dr. Pamela Gay and her minions at Astronomy Cast Live and UStream. Or just watch in the embedded player below. Here’s the schedule for Tuesday’s conferences:

9 a.m. PDT (12 noon EDT): Galaxy Discoveries
10:30 a.m. PDT (1:30 EDT): International Year of Astronomy 2009 Update from the AAS meeting.
12:40 pm PDT (3:40 EDT): Stars and Clusters

New Technique Reveals Ages of Millisecond Pulsars


Astronomers have developed a new technique to accurately determine the ages of millisecond pulsars, the fastest-spinning stars in the universe. The standard method for estimating pulsar ages is known to yield unreliable results, especially for the fast-spinning millisecond pulsars, said Bülent Kiziltan, a graduate student in astronomy and astrophysics at University of California Sant a Cruz. “An accurate determination of pulsar ages is of fundamental importance, because it has ramifications for understanding the formation and evolution of pulsars, the physics of neutron stars, and other areas,” he said.
Continue reading “New Technique Reveals Ages of Millisecond Pulsars”

Volcano Lahar

Lahar aftermath in Columbia

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Volcanoes have many ways to kill you, from hot lava, rocks blasted through the air, to poisonous gasses. But one of the most dangerous parts of a volcano are mud flows that can stream down their sides, following the path of river valleys. Volcano lahars have been the cause of many deaths in the last few centuries. With more people living close to or even on the flanks of steep volcanoes, even more deaths are certain.

Lahars are volcanic mudflows, and they don’t have to come directly from volcanic activity. They occur when huge amounts of volcanic ash, mixed with water flows down the side of a mountain. They can flow at speeds more than 100 km/hour, following the path of a river valley, but with the weight of concrete. Lahars are liquid when they’re flowing, and then harden almost solid when they stop. One cause of a volcano lahar is an eruption, when volcanic ash mixes with a volcano glacier, creating this muddy mixture. It’s also possible for a lahar to form when a lake or dam breaks, mixing water with ash already on the side of a volcano.

And they’ve caused terrible damage. The eruption of Nevado del Ruiz in Columbia in 1985 sent lahars down the mountainside, burying the city of Armero under 5 meters of mud and debris. A lahar coming off Mount Rainier in Washington sent a wall of mud 140 meters deep, covering a total area of 330 square kilometers – 300,000 people now live in the area covered by that lahar. In the recent eruption of Mount Pinatubo in 1991, 700 people were killed by the lahars that came down the mountain after the intense rainfall that followed the eruption.

The term lahar comes from the Indonesian word for “wave”.

We have written many article about volcanoes in Universe Today. Here’s an article about pyroclastic flows, and here’s an article Plinian eruptions which can cause pyroclastic flows.

Want more resources on the Earth? Here’s a link to NASA’s Human Spaceflight page, and here’s NASA’s Visible Earth.

We have also recorded an episode of Astronomy Cast about Earth, as part of our tour through the Solar System – Episode 51: Earth.

Astronomers Find New Way to Measure Cosmic Distances

Cepheid stars in galaxies such as M81, shown here. The stars could offer a new way to measure distances to objects in the universe. Image courtesy of Ohio State University.” width=”580″ height=”535″ class=”size-medium wp-image-32187″ />
hio State University astronomers are using the Large Binocular Telescope to look for ultra long period cepheid stars in galaxies such as M81, shown here. The stars could offer a new way to measure distances to objects in the universe. Image courtesy of Ohio State University.

Using a rare type of giant Cepheid variable stars as cosmic milemarkers, astronomers have found a way to measure distances to objects three times farther away in space than previously possible. Classical Cepheids are stars that pulse in brightness and have long been used as reference points for measuring distances in the nearby Universe. But astronomers have found a way to use “ultra long period” (ULP) Cepheid variables as beacons to measure distances up to 300 million light years and beyond.
Continue reading “Astronomers Find New Way to Measure Cosmic Distances”

Volcanoes in Mexico

Pico de Orizaba

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Mexico is known for its beaches and historical ruins, but did you know that Mexico has some of the most spectacular volcanoes in North America? It has the tallest volcano in North America (the third tallest mountain in North America), and islands formed from shield volcanoes.

Mexico Volcanoes

  • Barcena – a volcano on the island of San Benedicto that wiped out all life on the island in 1952.
  • Ceboruco – A volcano that had the largest eruption in Mexico in 930 AD.
  • Chichinautzin – A volcanic field just outside Mexico City.
  • Colima – An active volcano visible from Mexico City.
  • El Chichon – A previously unknown lava cone that erupted in 1982, killing 2000 people.
  • Jocotitlan Volcano – A distinct horseshoe-shaped volcano.
  • Nevado de Toluca – A dormant stratovolcano and Mexico’s 4th highest peak.
  • Paricutin – A volcano that appeared suddenly in a Mexican cornfield, rose to a height of more than 400 meters and then stopped growing.
  • Pico de Orizaba – A dormant volcano that hasn’t erupted since the 17th century, it’s the third tallest peak in North America.
  • Popocatepetl – An active volcano in Mexico, the 2nd tallest active volcano in North America.
  • San Martin – A shield volcano near the Gulf Coast of Mexico.
  • Socorro – a shield volcano that makes up the largest of the Revillagigedo Islands.
  • Tacana – A tall stratovolcano that straddles the border between Mexico and Guatemala

We have written many articles about volcanoes for Universe Today. Here’s an article about Costa Rica volcanoes, and here’s a full list of famous volcanoes around the world.

Want more resources on the Earth? Here’s a link to NASA’s Human Spaceflight page, and here’s NASA’s Visible Earth.

We have also recorded an episode of Astronomy Cast about Earth, as part of our tour through the Solar System – Episode 51: Earth.

Jocotitlan Volcano

Jocotitlan

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Jocotitlan is an stratovolcano located about 60 kilometers northwest of Mexico City. It rises to an elevation of 3,900 meters above sea level, but it’s isolated from any other mountains or peaks in the surrounding plains, rising up 1,300 meters above the Toluca basin.

One of its most prominent features is a horseshoe-shaped escarpment visible from the northeast; it formed when the northeast edge of the caldera collapsed. Whenever this event happened, it created an enormous landslide that buried 80 square kilometers of land to the northeast of the volcano.

Jocotitlan formed in the Pleistocene era (11,000 to 1.8 million years ago) primarily out of andesitic-to-dacitic lava flows. After that there was an obsidian dacitic eruptino and then the creation of a lava dome complex. The volcano produced regular lava flows, pumice-fall eruptions and pyroclastic surges. The last known eruption at Jocotitlan happened about 700 years ago, and produced block-and-ash flows and pyroclastic surges.

We have written many article about volcanoes for Universe Today. Here’s an article about other volcanoes in Mexico, and here’s an article about many famous volcanoes.

Want more resources on the Earth? Here’s a link to NASA’s Human Spaceflight page, and here’s NASA’s Visible Earth.

We have also recorded an episode of Astronomy Cast about Earth, as part of our tour through the Solar System – Episode 51: Earth.

Barcena Volcano

Barcena

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Barcena is a volcano located on the island of San Benedicto, the third largest island of the Revillagigedo Islands. The whole island is only about 4.8 km by 2.4 km and Barcena takes up a good chunk of the southern end. Barcena rises to an elevation of 332 meters, forming a volcanic crater.

There has only been on eruption from Barcena in recorded history, but it was a big one. On August 1, 1952, Barcena had a severe Vulcanian eruption measuring 3 on the Volcanic Explosivity Index. It released huge pyroclastic flows that rolled over the entire island, covering it in ash and pumice to a depth of 3 meters. Within less than 2 weeks, it had created a new volcanic cone more than 300 meters high. A second series of eruptions started up later in the year, releasing magma that broke out of the cone and flowed into the ocean. By late 1953, the volcano went dormant again.

The eruption wiped out all the plants and wildlife on the island, making the San Benedicto Rock Wren extinct. Within a few years the plants and wildlife made a return, although the island still looks barren.

We have written many article about volcanoes for Universe Today. Here’s an article about Tacana, a tall stratovolcano that straddles the border between Mexico and Guatemala. And here’s an article about Paricutin, a volcano that suddenly appeared in a farmer’s cornfield.

Want more resources on the Earth? Here’s a link to NASA’s Human Spaceflight page, and here’s NASA’s Visible Earth.

We have also recorded an episode of Astronomy Cast about Earth, as part of our tour through the Solar System – Episode 51: Earth.

Colima Volcano

Volcano Colima

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Colima is the name of a state in Mexico, as well as a city. But we’re going to be talking about another feature in Mexico, Colima’s Volcano. Colima is the most active volcano in Mexico, having erupted more than 40 separate times since records were first kept in 1576. The volcano stands at an elevation of 4,330 meters.

Geologists believe that Colima has been active for about 5 million years. Back in the Pleistocene era (between 11,000 and 1.8 million years ago), a huge earthquake triggered a landslide on the volcano, releasing 25 cubic kilometers of debris that traveled 120 km, reaching the Pacific Ocean. Major collapse events like this are believed to happen every few thousand years.

In the Colima volcano complex there are actually two different volcanoes. The older, dormant volcano is known as Nevado de Colima, and it stands at an elevation of 4330 meters. The younger, active volcano is known as the Volcan de Colima – Colima Volcano.

Colima has the potential to be a devastating volcano. There are about 300,000 people living within 40 km of the volcano. It has been chosen by scientists as a “Decade volcano”, and has been singled out for careful study to predict if and when a major eruptive event is happening. There have been several evacuations of the region over the last decade, since a large eruption or lava flow could affect an 11-kilometer radius around the volcano. In a 1999 eruption, Colima blasted out material that reached a distance of 5 km. Fortunately, lava flows from the volcano have never reached inhabited areas.

We have written many articles about volcanoes for Universe Today. Here’s an article about Popocatepeti, another volcano in Mexico. And here’s an article about Paricutin, a volcano that appeared in a cornfield in Mexico.

Want more resources on the Earth? Here’s a link to NASA’s Human Spaceflight page, and here’s NASA’s Visible Earth.

We have also recorded an episode of Astronomy Cast about Earth, as part of our tour through the Solar System – Episode 51: Earth.