Formation of Saturn

Solar nebula. Image credit: NASA

Like the rest of the planets, Saturn formed from the solar nebula about 4.6 billion years ago. This solar nebula started out as a vast cloud of cold gas and dust which was disturbed somehow – perhaps by colliding with another cloud, or the shock wave from a supernova.

You can also check out these cool telescopes that will help you see the beauty of planet Saturn.

The cloud compressed down, forming a protostar in the center, surround by a flattened disk of material. The inner part of this disk contained more heavier elements, and formed the terrestrial planets, while the outer region was cold enough for ices to remain intact.

These ices came together, forming larger and larger planetesimals. And these planetesimals collided together, merging into planets. At some point in Saturn’s early history, a moon roughly 300 km across might have been torn apart to create the rings that circle the planet today.

Since Saturn was smaller than Jupiter, it cooled down more quickly. Astronomers think that once its outer atmosphere reached about 15 K, helium condensed into droplets that fell towards its core. The friction from these droplets heated up the planet to the point that it gives off roughly 2.3 times the amount of energy it receives from the Sun.

Here’s an article from Universe Today about how the gas giant planets might have consumed their moons early on, and another article about how gas giant planets might form around other stars.

Here’s an article about the formation of Saturn’s rings, and an article about what Saturn’s moons might tell scientists about planet formation.

We have recorded two episodes of Astronomy Cast just about Saturn. The first is Episode 59: Saturn, and the second is Episode 61: Saturn’s Moons.

Radiation on Saturn

Radiation Belts on Saturn. Image credit: NASA/JPL/SSI

Just like Jupiter, Saturn radiates out more energy that it draws in from the Sun. In fact, Saturn radiates 2.3 times more energy than it receives from the Sun.

You can also check out these cool telescopes that will help you see the beauty of planet Saturn.

This has been a bit of a mystery to scientists. But the solution lies in the fact that Saturn’s atmosphere is relatively poor in helium, compared to Jupiter. Scientists think it cooled faster than Jupiter after initial formation, and then helium droplets formed when the temperature of the atmosphere dropped below 15 K. These droplets have been falling down into the core of Saturn, heating it up, and generating the heat.

When NASA’s Cassini first arrived at Saturn, the spacecraft detected lightning storms and radiation belts around the planet. It even found a brand new radiation belt located inside the rings of Saturn. The belts extend from about 139,000 km from Saturn’s center out to 362,000, and contain highly charged particles.

Here’s an article about Cassini finding the radiation belts around Saturn, and another about strange radio emissions coming from Saturn, related to the belts.

Here’s more information on the radiation belts, and a nice photograph from NASA.

We have recorded two episodes of Astronomy Cast just about Saturn. The first is Episode 59: Saturn, and the second is Episode 61: Saturn’s Moons.

Storms on Saturn

Storms on Saturn. Image credit: NASA/JPL/SSI

Jupiter is well known for the storms that rage across its upper atmosphere, especially the Great Red Spot. But Saturn has storms too. They’re not as large, intense or large lived, but compared to Earth, they’re enormous. And Saturn has one of the big mysteries in the Solar System; a hexagon-shaped storms at its poles.

You can also check out these cool telescopes that will help you see the beauty of planet Saturn.

Winds blow hard on Saturn. The highest velocities are near the equator, where easterly blowing winds can reach speeds of 1,800 km/h. The wind speeds drop off as you travel towards the poles.

Like Jupiter, storms can appear in the bands that circle the planet. One of the largest of these was the Great White Spot, observed by the Hubble Space Telescope in 1990. These storms seem to appear once every year on Saturn (once every 30 Earth years).

NASA’s Cassini spacecraft discovered static hexagonal storm circling around Saturn’s north pole, including a clearly defined eyewall – just like a hurricane. Each side on the northern polar hexagon is approximately 13,800 km long, and the whole structure rotates once every 10 hours and 39 minutes; the same as a day on Saturn.

Here’s an article about a time when Cassini tracked a long-lived lightning storm on Saturn, and another about the strange “Dragon Storm” seen in the planet’s southern hemisphere.

Here’s an article about the northern hexagonal storm from MSNBC, and Astronomy Picture of the Day has an image of storm alley on Saturn.

We have recorded two episodes of Astronomy Cast just about Saturn. The first is Episode 59: Saturn, and the second is Episode 61: Saturn’s Moons.

Mass of Saturn

Cassini's view of Saturn. Image credit: NASA/JPL/SSI

The mass of Saturn is 5.6846×1026 kg. Just for a comparison, this is 95 times the mass of the Earth.

Saturn is much larger than Earth; its equator spans 9.4 times the size of our home planet. And yet, it’s much less dense. In fact, Saturn has such a low density that it would actually float on water if you could find a pool large enough.

And so, even though it’s much larger and more massive than Earth, if you could actually stand on the “surface of Saturn” – which you can’t, there’s no surface – you would only feel 91% of gravity that we feel here on Earth.

Here’s an article from Universe Today explaining just how big planets can get, and an article about how Jupiter and the other gas giants might have gobbled up their moons while they were forming.

Here’s Hubblesite’s News Releases about Saturn, which has more info about the ringed planet, and NASA’s Solar System Exploration guide.

We have recorded two episodes of Astronomy Cast just about Saturn. The first is Episode 59: Saturn, and the second is Episode 61: Saturn’s Moons.

Is There Life on Saturn?

Color view of Enceladus. Image credit: NASA/JPL/SSI

It’s hard to imagine a planet less hospitable for life than Saturn. The planet is comprised almost entirely hydrogen and helium, with only trace amounts of water ice in its lower cloud deck. Temperatures at the top of the clouds can dip down to -150 C.

You can also check out these cool telescopes that will help you see the beauty of planet Saturn.

Temperatures do get warmer as you descend into Saturn’s atmosphere, but the pressures increase too. When temperatures are warm enough to have liquid water, the pressure of the atmosphere is the same as several kilometers beneath the ocean on Earth.

To find life, scientists will want to take a good look at Saturn’s moons. They’re comprised of significant amounts of water ice, and their gravitational interaction with Saturn probably keeps their interiors warm. Saturn’s moon Enceladus is known to have geysers of water erupting from its southern pole. It’s possible that it has vast reserves of superheated water beneath an ice crust.

And Saturn’s moon Titan has lakes and seas of hydrocarbons, thought to be the precursors of life. In fact, scientists think that Titan is very similar in composition to the Earth’s early history.

Hydrocarbons have even been detected across the surface of Saturn’s moon Hyperion.

There might not be life on Saturn, but there are enough intriguing locations to explore around the ringed planet to keep astronomers busy for years.

Here’s an article about exotic life that could live on Titan, and another that dismisses the possibility that there’s life on Enceladus.

This is an article from the Guardian about the possibility of life on Enceladus, and hydrocarbons on Hyperion.

We have recorded two episodes of Astronomy Cast just about Saturn. The first is Episode 59: Saturn, and the second is Episode 61: Saturn’s Moons.

How Old is Saturn?

Color view of Saturn. Image credit: NASA/JPL/SSI

Saturn formed with the rest of the planets 4.6 billion years ago, out of a spinning disk of gas and dust. This dust collapsed down to form the Sun, and planets formed out of the disk around it. This is why all of the planets orbit the Sun in the same direction.

That’s the easy question.

You can also check out these cool telescopes that will help you see the beauty of planet Saturn.

The more complicated question is, how old are Saturn’s rings? Some parts might be almost as old as the Solar System, but others are being continuously refreshed. The primary theory for the formation of Saturn’s Rings is that a 300 km moon was torn apart by Saturn’s gravity into the ring system that we see today. But that probably happened more than 4 billion years old.

But Saturn’s rings are bright, and almost made of pure water ice. Since infalling dust should have darkened the rings, they might be as young as 100 million years old. Or perhaps they are ancient, but regular collisions between ring objects keep them looking fresh and new.

One interesting note. Astronomers think that the composition of Saturn – 88% hydrogen and 11% helium with other trace elements – almost exactly matches the composition of the early solar nebula. Saturn is like a miniature version of the Solar System.

Here’s an article from Universe Today that discusses how Saturn’s rings could be as old as the Solar System, and another article about how gas giant planets might have consumed many of their moons early on in their history.

Ask an Astronomer has another answer to this question, and another look at the age of the rings from Geology.com.

We have recorded two episodes of Astronomy Cast just about Saturn. The first is Episode 59: Saturn, and the second is Episode 61: Saturn’s Moons.

Is There Water on Saturn?

Saturn's moon Enceladus behind the rings. Image credit: NASA/JPL/SSI

Saturn is almost entirely hydrogen and helium, but it does have trace amounts of other chemicals, including water. When we look at Saturn, we’re actually seeing the upper cloud tops of Saturn’s atmosphere. These are made of frozen crystals of ammonia.

You can also check out these cool telescopes that will help you see the beauty of planet Saturn.

But beneath this upper cloud layer, astronomers think there’s a lower cloud deck made of ammonium hydrosulfide and water. There is water, but not very much.

Once you get away from Saturn itself, though, the nearby area has plenty of water. Saturn’s rings are almost entirely made of water ice, in chunks ranging in size from dust to house-sized boulders.

And all of Saturn’s moons have large quantities of water ice. For example, Saturn’s moon Enceladus is thought to have a mantle rich in water ice, surrounding a silicate core. Geysers of water vapor were detected by NASA’s Cassini spacecraft, spraying out of cracks at Enceladus’ southern pole.

If you want to look for water at Saturn, don’t look at the planet itself, but there’s water all around it.

Here’s an article from Universe Today about the plume of water ice coming off of Enceladus, and how Saturn’s environment is driven by ice.

Here’s an article from NASA about the composition of ice at Saturn’s moon Rhea, and the discovery of liquid water on Enceladus.

We have recorded two episodes of Astronomy Cast just about Saturn. The first is Episode 59: Saturn, and the second is Episode 61: Saturn’s Moons.

Theory of Relativity Passes Another Test

Einstein’s theory of General Relativity has been around for 93 years, and it just keeps hanging in there. With advances in technology has come the ability to put the theory under some scrutiny. Recently, taking advantage of a unique cosmic coincidence, as well as a pretty darn good telescope, astronomers looked at the strong gravity from a pair of superdense neutron stars and measured an effect predicted by General Relativity. The theory came through with flying colors.

Einstein’s 1915 theory predicted that in a close system of two very massive objects, such as neutron stars, one object’s gravitational tug, along with an effect of its spinning around its axis, should cause the spin axis of the other to wobble, or precess. Studies of other pulsars in binary systems had indicated that such wobbling occurred, but could not produce precise measurements of the amount of wobbling.

“Measuring the amount of wobbling is what tests the details of Einstein’s theory and gives a benchmark that any alternative gravitational theories must meet,” said Scott Ransom of the National Radio Astronomy Observatory.

The astronomers used the National Science Foundation’s Robert C. Byrd Green Bank Telescope (GBT) to make a four-year study of a double-star system unlike any other known in the Universe. The system is a pair of neutron stars, both of which are seen as pulsars that emit lighthouse-like beams of radio waves.

“Of about 1700 known pulsars, this is the only case where two pulsars are in orbit around each other,” said Rene Breton, a graduate student at McGill University in Montreal, Canada. In addition, the stars’ orbital plane is aligned nearly perfectly with their line of sight to the Earth, so that one passes behind a doughnut-shaped region of ionized gas surrounding the other, eclipsing the signal from the pulsar in back.

Animation of double pulsar system

The eclipses allowed the astronomers to pin down the geometry of the double-pulsar system and track changes in the orientation of the spin axis of one of them. As one pulsar’s spin axis slowly moved, the pattern of signal blockages as the other passed behind it also changed. The signal from the pulsar in back is absorbed by the ionized gas in the other’s magnetosphere.

The pair of pulsars studied with the GBT is about 1700 light-years from Earth. The average distance between the two is only about twice the distance from the Earth to the Moon. The two orbit each other in just under two and a half hours.

“A system like this, with two very massive objects very close to each other, is precisely the kind of extreme ‘cosmic laboratory’ needed to test Einstein’s prediction,” said Victoria Kaspi, leader of McGill University’s Pulsar Group.

Theories of gravity don’t differ significantly in “ordinary” regions of space such as our own Solar System. In regions of extremely strong gravity fields, such as near a pair of close, massive objects, however, differences are expected to show up. In the binary-pulsar study, General Relativity “passed the test” provided by such an extreme environment, the scientists said.

“It’s not quite right to say that we have now ‘proven’ General Relativity,” Breton said. “However, so far, Einstein’s theory has passed all the tests that have been conducted, including ours.”

Original News Source: Jodrell Bank Observatory

MESSENGER Provides New Insights on Mercury

mercury_plains..Credit: NASA/JHUAP/Arizona State University

Data from the MESSENGER spacecraft’s first flyby of Mercury in January of 2008 are now turning into science results. Several scientists discussed their findings at a press conference today highlighting the MErcury Surface, Space ENvironment, GEochemistry, and Ranging mission, the first spacecraft to visit Mercury since NASA’s Mariner 10 made three flyby passes in 1974 and 1975. Among the findings, scientists discovered volcanism has played a more extensive role in shaping the surface of Mercury than previously thought. MESSENGER data has also identified and mapped surface rock units that
correspond to lava flows, volcanos, and other geological features, showing an apparent planet-wide iron deficiency in Mercury’s surface rocks. Additionally, other instruments made the first observations about the surface and atmospheric composition of the closest world to the sun.

“We have now imaged half of the part of Mercury that was never seen by Mariner 10,” says Mark S. Robinson of Arizona State University, lead author of s study on composition variations in Mercury’s surface rocks using their multispectral colors. “The picture is still incomplete, but we’ll get the other half on October 6th.”

MESSENGER will make two more Mercury flybys (October 6, 2008 and September 29, 2009) before
going into orbit around the planet, March 18, 2011.

MESSENGER’s big-picture finding, says Robinson, is the widespread role played by volcanism. While impact craters are common, and at first glance Mercury still resembles the Moon, much of the planet has been resurfaced through volcanic activity.

“For example, according to our color data the Caloris impact basin is completely filled with smooth plains material that appears volcanic in origin,” Robinson explains. “In shape and form these deposits are very similar to the mare basalt flows on the Moon. But unlike the Moon, Mercury’s smooth plains are low in iron, and thus represent a relatively unusual rock type.”

Mercury’s surface also has a mysterious, widespread low-reflective material Robinson says, “It’s an important and widespread rock that occurs deep in the crust as well as at the surface, yet it has very little ferrous iron in its silicate minerals.”

Another experiment measured the charged particles in the planet Mercury’s magnetic field, which enabled the first observations about the surface and atmospheric composition of Mercury. “We now know more about what Mercury’s made of than ever before,” said Thomas Zurbuchen, a professor at the University of Michigan. “Holy cow, we found way more than we expected!”

Zurbuchen is project leader of the Fast Imaging Plasma Spectrometer (FIPS), a soda can-sized sensor on board the MESSENGER spacecraft.

FIPS detected silicon, sodium, sulfur and even water ions around Mercury. Ions are atoms or molecules that have lost electrons and therefore have an electric charge.

Because of the quantities of these molecules that scientists detected in Mercury’s space environment, they surmise that they were blasted from the surface or exosphere by the solar wind. The solar wind is a stream of charged particles emanating from the sun. It buffets Mercury, which is 2/3 closer to the sun than the Earth, and it causes particles from Mercury’s surface and atmosphere to sputter into space. FIPS measured these sputtered particles.

Mercury and MESSENGER form the subject of 11 papers in a special section devoted to the January flyby in the July 4, 2008, issue of the scientific journal Science.

News Sources: University of Arizona, MESSENGER site

Seasons on Saturn

Collage showing the change in seasons on Saturn. Credit: NASA/ESA/Hubble

Like Earth, Saturn’s axis is tilted relative to the Sun’s equator – 27-degrees on Saturn, compared to 23-degrees for Earth. And this tilt is very easy to see, because Saturn’s rings extend out from its equator. There are times during its orbit when we see Saturn’s rings fully extended, and other times when the rings are just a thin line, seen edge on.

You can also check out these cool telescopes that will help you see the beauty of planet Saturn.

You can also check out these cool telescopes that will help you see the beauty of planet Saturn.

Since Saturn takes 30 years to orbit the Sun, so it’s seasons are much, much longer than Earth’s. Each of the planet’s hemispheres take turns soaking up radiation from the Sun, heating up. When the rings are fully facing the Sun, they can shade the planet, and further decrease the amount of energy received by the hemisphere experiencing winter.

And these seasons do have an impact on the planet’s weather. Over the course of 20 years, scientists recorded that wind speeds around Saturn’s equatorial regions decreased by about 40%. NASA’s Voyager flybys in 1980-81 detected wind speeds of 1,700 km/h, while they were only going about 1,000 km/h in 2003.

Here’s an article from Universe Today about how Saturn’s weather changes over long periods, and the discovery of a cyclone at the planet’s north pole.

Astronomy Picture of the Day has a beautiful image of Saturn’s changing seasons, and an article from BBC about the planet’s changing wind speeds.

We have recorded two episodes of Astronomy Cast just about Saturn. The first is Episode 59: Saturn, and the second is Episode 61: Saturn’s Moons.