Showing posts with label sun. Show all posts
Showing posts with label sun. Show all posts

The Origins of The Solar System

We live in a universe of almost unimaginable size. To give you an idea of the scale, we can only use optical and radio methods to observe objects out to about 13,000 million light years away and nobody knows what lies beyond that. Closer to us we can see clusters of galaxies at distances out to about 750 million light years. The other galaxies of what is know as the Local Group of galaxies are all within 2.5 million light years of us. These galaxies are composed of millions and billions of stars.

Our own galaxy, the Milky Way, is a typical spiral galaxy. This means is looks like a great swirling whirlpool with spiral arms extending out from the center. The Milky Way galaxy is 100,000 light years in diameter and our own star, the Sun, lies on the edge of one of the spiral arms. The Sun is about 30,000 light years from the center of the Milky Way galaxy and takes 225 million years to complete one orbit around the galactic center.

According to modern scientific theory the star we call the Sun was formed about 4,500 million years ago. The Solar System originated when gravitational forces caused what is called the solar nebula to collapse and coalesce into a spinning disc with the central mass forming the Sun. The planets formed from large clouds of gas and dust which gradually built up over million of years as they orbited the central mass of the disc.

The central mass continued to build up in size and as it did the gravitational field it exerted grew stronger. As the gravitational field grew stronger the central mass pulled in more gas and dust and grew even larger.

Eventually, the gravitational force became so powerful that the temperature and pressure at the center of the mass rose high enough to cause hydrogen atoms to undergo fusion into helium atoms. This fusion reaction releases enormous amounts of energy and is the source of the Suns power.

Now illuminated by the Suns rays, the planets of our solar system continued to form and transform. All of the planets have undergone a great deal of change since they first accreted. These changes were brought about in a variety of ways, including violent collisions which resulted in craters that can still be seen today. The planets also went through changes caused by volcanism, melting, structural deformation and the release of gases from deep within.

The planets of our Solar System are generally divided into two groups. The inner planets, which include Mercury, Venus, Earth and Mars and the outer planets, Jupiter, Saturn, Uranus, Neptune and until recently the Dwarf Planet Pluto. The inner planets are all characterized by having solid surfaces and are relatively small compared to the outer planets. The outer planets are all characterized by not having a solid surface and are often referred to as gas giants. The inner and outer planets are also separated by a band of asteroids orbiting between Mars and Jupiter.

Comets, meteors and asteroids can also be found orbiting the sun in large numbers from the outer reaches of the Solar System to very close to the Sun. Comets are balls of frozen liquids and dust which often follow eccentric orbits for outside the orbit of Dwarf Planet Pluto and only display their characteristic tails when their orbit brings them closer to the Sun. Asteroids and meteors are both made mainly of rock. The difference between asteroids and meteors is their size, meteors can be as small a grain of dust, asteroids can be miles in diameter and are sometimes called planetoids.

At the outer fringes of the Solar System beyond the orbit of Neptune is the Kuiper belt where at least three dwarf planets orbit. They are Ceres, Pluto and Eris and they are accompanied by millions of smaller objects about which little is known. At this time a variety of spacecraft are either on their way to the far reaches of the Solar System or are planned for the near future. It will be fascinating to see what wonders these space probes will tell us about the Solar System we call home.

The Star We Call The Sun

The Sun is called Sol in Latin and that is where the term Solar System comes from. It is a typical main-sequence star and is by far the largest and most massive object in our Solar System. The Sun contains 99.8 percent of all the matter in the Solar System with the planet Jupiter taking up most of the rest. The Sun is a population one, GV2 class star and is sometimes referred to as a typical star and that is true in many respects. However the Sun is actually larger than most of the other stars in the same class as the Sun.

The Sun is composed of 74 percent hydrogen, 25 percent helium and traces of other elements. The temperature at the Suns core which is considered the inner 20 percent, is approximately 15.6 million degrees Kelvin, the pressure is 250 billion atmospheres and the mass density is more than 150 times that of water. Under such extreme conditions nuclear fusion takes place where by hydrogen atoms are combined to from helium atoms. This reaction releases massive amounts of energy in the form of gamma rays and is responsible for the Suns 386 billion billion megawatt power output. During the course of their journey out to the surface these gamma rays are repeatedly absorbed and re-emitted at lower and lower temperatures. By the time the energy reaches the surface is has been reduced to mostly visible light and is carried through the last part of the way more by convection than radiation.

The convection zone is the Suns outer layer down to about 70 percent of the Suns radius. It is an area where thermal convection takes place in the form of great thermal columns. These thermal columns are heated by nuclear fusion taking place in the Suns core and rise up to the Suns surface where they release their energy out into space in the form of sunlight and particles. As the thermal columns discharge their energy they cool and sink back down in the Suns interior where they are reheated and back up to surface again in a great cycle. The tops of these great thermal columns can be seen on the surface of the Sun in the form of what is called solar granulation and supergranulation.

The surface layer of the Sun that we can see is called the photosphere and has a temperature of about 5800 degrees Kelvin. Above the photosphere are five layers that compose the Suns atmosphere. They are the temperature minimum, the chromosphere, the transition region, the corona and the heliosphere. The temperature minimum region extends from the photosphere up to 2000 kilometers and has a temperature of about 4000 degrees Kelvin. This is cool enough for molecules such as water and carbon monoxide to exist and they can be detected by their absorption spectra.

The chromosphere extends from the top of the temperature minimum region up another 2000 kilometers and is named for the Greek word chromo which means color. The chromosphere can be seen as a flash of color right at the start and the end of a total solar eclipse of the Sun. Strangely enough, the temperature of the chromosphere gradually increases with altitude up to about 100,000 degrees Kelvin at the top.

Above the chromosphere is a transition region where the temperature rises rapidly to about one million degrees Kelvin. This temperature increase is caused by what is known as a phase transition of the element helium present in the transition region. The transition region does not have a well defined altitude and is in constant motion. The transition region is not easily seen from Earth but can be observed by space based instruments operating in the far ultraviolet region of the spectrum.

After the chromosphere is the corona which is much larger than the previous layers of the Suns atmosphere and extends far out into space. The corona is characterized by solar prominences which are immense clouds of super heated glowing gas that has erupted from the upper chromosphere. The corona can be clearly seen during total eclipses of the Sun and is very spectacular to see. The corona is composed of charged particles that become what we call the solar wind as they radiate outward from the Sun at 450 kilometers per second and are responsible for the aurora borealis.

Beyond the corona is the heliosphere which is also know as the magnetosphere. The heliosphere is immensely strong and extends far beyond the orbit of the dwarf planet Pluto. The solar wind travels outward along the heliosphere until it collides with the helipads about 50 astronomical units from the Sun.

When observed with the proper filters we can see sunspots on the surface of the Sun. These spots have a lower temperature than the surrounding area and therefore appear dark. Sunspots are areas of intense magnetic power where thermal convection from the interior of the Sun has been inhibited. Sunspots usually form pairs with opposite magnetic polarity and are responsible for solar flares. The number of sunspots varies over the course of an eleven year solar cycle.

The Sun has been active for about four and a half billion years and has used up about half of the hydrogen fuel it started with. The Sun will continue to burn for about another five billion years after which it will start to force helium to under go nuclear fusion into heavier elements. This will cause the Sun to swell up in size to the point of consuming the Earth and more as it becomes what is called a red giant. A billion years after becoming a red giant our Sun will finally collapse into a white dwarf. Incredibly, it could then take as much as one trillion years to cool off.

The Origins of The Solar System

We live in a universe of almost unimaginable size. To give you an idea of the scale, we can only use optical and radio methods to observe objects out to about 13,000 million light years away and nobody knows what lies beyond that. Closer to us we can see clusters of galaxies at distances out to about 750 million light years. The other galaxies of what is know as the Local Group of galaxies are all within 2.5 million light years of us. These galaxies are composed of millions and billions of stars.

Our own galaxy, the Milky Way, is a typical spiral galaxy. This means is looks like a great swirling whirlpool with spiral arms extending out from the center. The Milky Way galaxy is 100,000 light years in diameter and our own star, the Sun, lies on the edge of one of the spiral arms. The Sun is about 30,000 light years from the center of the Milky Way galaxy and takes 225 million years to complete one orbit around the galactic center.

According to modern scientific theory the star we call the Sun was formed about 4,500 million years ago. The Solar System originated when gravitational forces caused what is called the solar nebula to collapse and coalesce into a spinning disc with the central mass forming the Sun. The planets formed from large clouds of gas and dust which gradually built up over million of years as they orbited the central mass of the disc.

The central mass continued to build up in size and as it did the gravitational field it exerted grew stronger. As the gravitational field grew stronger the central mass pulled in more gas and dust and grew even larger.

Eventually, the gravitational force became so powerful that the temperature and pressure at the center of the mass rose high enough to cause hydrogen atoms to undergo fusion into helium atoms. This fusion reaction releases enormous amounts of energy and is the source of the Suns power.

Now illuminated by the Suns rays, the planets of our solar system continued to form and transform. All of the planets have undergone a great deal of change since they first accreted. These changes were brought about in a variety of ways, including violent collisions which resulted in craters that can still be seen today. The planets also went through changes caused by volcanism, melting, structural deformation and the release of gases from deep within.

The planets of our Solar System are generally divided into two groups. The inner planets, which include Mercury, Venus, Earth and Mars and the outer planets, Jupiter, Saturn, Uranus, Neptune and until recently the Dwarf Planet Pluto. The inner planets are all characterized by having solid surfaces and are relatively small compared to the outer planets. The outer planets are all characterized by not having a solid surface and are often referred to as gas giants. The inner and outer planets are also separated by a band of asteroids orbiting between Mars and Jupiter.

Comets, meteors and asteroids can also be found orbiting the sun in large numbers from the outer reaches of the Solar System to very close to the Sun. Comets are balls of frozen liquids and dust which often follow eccentric orbits for outside the orbit of Dwarf Planet Pluto and only display their characteristic tails when their orbit brings them closer to the Sun. Asteroids and meteors are both made mainly of rock. The difference between asteroids and meteors is their size, meteors can be as small a grain of dust, asteroids can be miles in diameter and are sometimes called planetoids.

At the outer fringes of the Solar System beyond the orbit of Neptune is the Kuiper belt where at least three dwarf planets orbit. They are Ceres, Pluto and Eris and they are accompanied by millions of smaller objects about which little is known. At this time a variety of spacecraft are either on their way to the far reaches of the Solar System or are planned for the near future. It will be fascinating to see what wonders these space probes will tell us about the Solar System we call home.

Saturn is Visible Without Using a Telescope

Saturn, the sixth planet from the Sun, has the most spectacular set of rings in the solar system. Saturn has been known since prehistoric times. Saturn is visibly flattened (oblate) when viewed through a small telescope; its equatorial and polar diameters vary by almost 10% (120,536 km vs. Saturn also exhibits long-lived ovals (red spot at center of image at right) and other features common on Jupiter. Saturn's rings remained unique in the known solar system until 1977 when very faint rings were discovered around Uranus (and shortly thereafter around Jupiter and Neptune). Saturn is the least dense of the planets; its specific gravity (0. Saturn is visibly flattened (oblate) when viewed through a small telescope; its equatorial and polar diameters vary by almost 10% (120,536 km vs.

Rings

Rings are 270,000 km in diameter, but only a few hundred meters thick. Early observations of Saturn were complicated by the fact that the Earth passes through the plane of Saturn's rings every few years as Saturn moves in its orbit. Saturn's rings are extraordinarily thin: though they're 250,000 km or more in diameter they're less than one kilometer thick. Two prominent rings (A and B) and one faint ring (C) can be seen from the Earth. The origin of the rings of Saturn (and the other jovian planets) is unknown. The current set of rings maybe only a few hundred million years old.

Satellites

The rings and the larger satellites are visible with a small astronomical telescope. There are satellites within the rings which result in the gaps that are present between some rings. Though they may have had rings since their formation, the ring systems are not stable and must be regenerated by ongoing processes, perhaps the breakup of larger satellites. Saturn has at least 35 naturally occurring satellites. All five, like the newly discovered four outer moons of Saturn, are irregular satellites.

Saturn's interior is hot (12000 K at the core) and Saturn radiates more energy into space than it receives from the Sun. Saturn's rings, unlike the rings of the other planets, are very bright (albedo 0. Saturn is the most oblate (flattened) planet in our Solar System. Saturn's outermost ring, the F-ring, is a complex structure made up of several smaller rings along which "knots" are visible. Saturn also exhibits long-lived ovals (red spot at center of image at right) and other features common on Jupiter. Saturn's bright rings are made of ice chunks (and some rocks) that range in size from the size of a fingernail to the size of a car. Saturn is visible without using a telescope, but a low-power telescope is needed to see its rings. Saturn is the only planet in our Solar System that is less dense than water. Saturn's auroral displays are caused by an energetic wind from the Sun that sweeps over the planet, much like Earth's aurora, which is occasionally seen in the nighttime sky.

A Tiny Blue Dot In Space

The late Dr. Stephen Jay Gould, a biologist and History of Science Professor at Harvard University, once noted that "The history of life is not necessarily progressive; it is certainly not predictable. The Earth's creatures have evolved through a series of contingent and fortuitous events."

Our Milky Way Galaxy is also the domicile of 100 billion stars in addition to our own golden, incandescent Sun. Our Star is situated very far from the heart of our Galaxy, where most of the other stars dwell, and where our own supermassive black hole--that weighs millions of times more than the Sun--resides in quiet, though restless, slumber, only to awaken now and then to hungrily devour bits of gas and star-stuff that wander too close to its maw. Our little luminous yellow Star is located halfway to the edge of the Milky Way along the Orion Spiral Arm.

Our Sun is circling around the center of the Milky Way at the speed of half a million miles per hour. Nevertheless, it takes about 200 million years for it to travel around once. Like other spiral galaxies, suspended like gigantic starlit pinwheels in Space, our Milky Way sports a bulge, a disk, and a dark matter halo. Dark matter is mysterious stuff, probably composed of some as-yet unidentified exotic particles that do not interact with light. This is why the dark matter is invisible, making its presence known only by its gravitational interactions with the luminous matter, that we can see.

Although the bulge, disk, and dark matter halo are all components of the same Galaxy, each contains different populations of objects. The halo and central bulge primarily host elderly stars, while the disk is filled with gas, dust, and much more bouncy, youthful stars. Our Sun is, currently, a member of the younger--or, at least, middle-aged--population, at less than 5 billion years of age. The Milky Way Galaxy itself is at least 5 billion years older than that. Our Galaxy is at a minimum 10 billion years old--and it is probably older. In fact, it might be one of the oldest galaxies in the Universe.

It is possible today for astrophysicists to determine the ages of certain stars. Specifically, this means that they can measure the amount of time that has elapsed since these stars were born as the outcome of condensation in dense knots studding huge, dark, frigid, interstellar molecular clouds composed of gas and dust. Some stars are quite youthful--for stars, that is--and are mere bouncing babies at "only" a few million years of age, or less. For example, such extremely young stars dance around happily in the "nearby" Orion Nebula. Our Sun and its family of planets, moons, and assorted other objects, formed about 4.56 billion years ago. However, many of the stars in our Galaxy were born much earlier!

Our tiny blue planet was born from an accretion disk revolving around the ancient Sun almost 5 billion years ago. About 4.53 billion years ago, the Earth and a Mars-sized object, sometimes called Theia, are thought to have crashed into one another, launching a multitude of moonlets into orbit around the ancient Earth. Eventually, these moonlets coalesced to form the Moon. The irresistible gravitational attraction of the newly-born Moon stabilized the Earth's fluctuating axis of rotation and set the stage for the conditions that were so necessary for the emergence of life. Long ago, the Moon was much closer to Earth than it is now. About 4.1 billion years ago, the surface of Earth finally cooled sufficiently for the crust to solidify--up until that time, both Earth and its newborn Moon were probably covered by global oceans of fiery magma. Also, at around this time, the atmosphere and the oceans of our planet formed.

The magic occurred sometime around 3.7 billion years ago. This was when the earliest and most primitive self-replicating nucleic acid tidbits emerged on our planet, probably derived from ribonucleic acid (RNA) molecules. The replication of these very primitive tidbits demanded energy; sufficient space to develop; and smaller, even more elementary, constituent building blocks. This necessary space was very rapidly used up by the flourishing brand new tidbits.. This resulted in bitter competition. Natural selection favored those molecules which were most efficient at propagating their own kind. Self-replicating material, in the form of deoxyribonucleic acid (DNA) molecules ultimately took over as the most efficient replicators. They quickly developed within enveloping membranes, which provided the stable and nurturing environment so necessary for them to continue replication.

About 3.9 billion years ago, the Late Heavy Bombardment occurred. This was when the greatest number of showering objects pelted the four inner planets: Mercury, Venus, our Earth, and Mars. The objects were probably comets, tossed out of their distant home that was situated beyond the outermost planet, Neptune, in what is called the Kuiper belt. These rudely evicted comets invaded the balmy inner Solar System, wreaking havoc as they rampaged through it. The invading comets of the Late Heavy Bombardment had likely been unceremoniously tossed out of their remote home as a result of the gymnastics engaged in by the giant outer planets--Jupiter, Saturn, Uranus and Neptune--which hurled them into the inner realm of our Solar System. This persistent shower of destructive, traveling chunks of alien ice and rock, possibly killed off any life that had already evolved, as the oceans boiled away. However, the theory of Panspermia suggests that life may have been transported to Earth by such rampaging meteorites. Of the two scenarios, however, the former is the most likely, and most (if not all) life existing on Earth prior to the Late Heavy Bombardment was extinguished.

Sometime between the Late Heavy Bombardment and 2.5 billion years ago, the very first precious and delicate tiny tidbits of life appeared. These fragile cells used carbon dioxide as a carbon source, and they were also adept at oxidizing inorganic materials to extract the necessary energy. Eventually, these fragile cells developed the ability to perform glycolysis. Glycolysis is a chemical process that liberates the energy of organic molecules such as glucose, and it generates Adenosine-5'-triphosphate (ATP) molecules as short-term energy sources. ATP continues to be used by almost all organisms on Earth, virtually unchanged, to this day.

About 3.5 billion years ago the very last universal ancestor of all the species now living on Earth existed. At this time, a split occurred between Bacteria and Archaea. Bacteria went on to generate ATP.

Photosynthesizing cynanobacteria evolved about 3 billion years ago. These minute bits of life used water as a reducing agent thereby producing oxygen as a waste product! The oxygen that was first oxidized dissolved iron in the oceans, manufacturing iron ore. The oxygen concentration in Earth's atmosphere subsequently rose, and poisoned many of the existing forms of bacteria. The Moon, at this time, was still very close to Earth, appearing as an enormous companion world in the sky--and it caused tides that were 1,000 feet high. The Earth was also continually subjected to extremely strong, hurricane force winds. Both of these occurrences resulted in a great deal of mixing and shaking that is believed to have enhanced evolutionary processes.

The first known footprints on land date to about 530 million years ago. This suggests that animal migrations onto the land from the oceans might have predated the evolution of terrestrial plants. About 475 million years ago, the first plants moved onto land. These primitive plants evolved from green algae that accumulated around the edges of ancient lakes. The first primitive plants were joined in their migration by fungi, which may have aided the invasion of land through symbiosis.

About 363 million years ago, our Earth began to look like home. Insects skittered over the land, and would soon evolve wings and flutter through the air. Sharks roamed the ancient seas with predatory intent. Vegetation covered what was once barren and desolate land with lovely seed-bearing plants. Beautiful, dense forests began to flourish. Four-limbed tetrapods started to adapt to terrestrial life. This era marks the triumphant Great Crawl, when our ancestors that still dwelled in ancient seas, heroically took their first tentative steps out from the water on to the land. Millions of years later, some of the heroic descendants of those brave little creatures would leave their footprints in the dust of the now much more distant Moon.

About 65.5 million years ago, the catastrophic Cretacious-Tertiary Extinction occurred. The disaster killed off about 50% of the animal species on Earth, including all non-avian dinosaurs. This event is believed to have been caused by the impact of a very large asteroid or comet that blasted out a huge crater in the Yucatan. The birds of the modern world are the descendants of those remnant species of avian dinosaurs that were able to survive this event.

About 14,000 years ago, during the so-called Anthropocene period, human beings evolved to attain their present dominant role over other species.

In August 2012, astronomers around the world celebrated the 35th anniversary of the launch of the Voyager 2 spacecraft. This hearty spacecraft would be the first--and so far only--craft to make the long journey to the two dazzling blue and green, remote ice-giant planets, Uranus and Neptune. Voyager 2, and its sister spacecraft, Voyager 1 (launched 16 days after Voyager 2), are still out there exploring, streaking away from our Sun, zipping out to the edge of our Solar System--and beyond. Scientists are breathlessly awaiting the moment when the sister crafts zoom out to the other side--tearing into interstellar space!

"Even 35 years on, our rugged Voyager spacecraft are poised to make new discoveries as we eagerly await the signs that we've entered interstellar space," Dr. Ed Stone told the press on August 21 2012. Dr. Stone is Voyager project scientist at the California Institute of Technology in Pasadena. He added that "Voyager results turned Jupiter and Saturn into full, tumultuous worlds, their moons from faint dots into distinctive places, and gave us our first glimpses of Uranus and Neptune up-close. We can't wait for Voyager to turn our models of the space beyond our Sun into the first observations from interstellar space."

On February 14, 1990, NASA commanded the Voyager 1 spacecraft to photograph the planets of our Solar System. One image that Voyager 1 returned was that of our Earth, taken from a record distance of "more than 4 billion miles". The fuzzy photograph shows a "pale blue dot" dangling like a tiny spherical bead against an almost incomprehensibly expansive and barren blackness.

In a commencement address delivered on May 11, 1996, the late Dr. Carl Sagan of Cornell University, told of his own thoughts on the deeper meaning of the historic photograph: "Look again at that dot... On it everyone you love, everyone you know, everyone you ever heard of, every human being who ever was, lived out their lives... It has been said that astronomy is a humbling and character-building experience. There is perhaps no better demonstration of the folly of human conceits than this distant image of our tiny world. To me, it underscores our responsibility to deal more kindly with one another, and to preserve and cherish the pale blue dot, the only home we've ever known."