You too can be an Amateur Astronomer!

One night, if you have some time and a set of binoculars handy, why not take a moment and check out Jupiter? Looking at Jupiter through binoculars can be a rewarding experience, if only because chances are you'll see a few of the Jovian moons. I recommend using one of the many of amateur astronomy apps to help you find Jupiter with your phone. You'll know it when you find it because Jupiter is the third brightest object in the night sky after the Moon and Venus. Then, holding your binoculars as steady as possible, take a look. What you will see is something like the image to the right. Jupiter will be a disk of light rather than a point (an indication it's "relatively" nearby). Also, you should see a few moons (if you're lucky 4). The moons will appear as small points of light in a line. Now is a pretty good time of year to observe Jupiter. For some extra motivation, here is some information about Jupiter and its moons.
Jupiter

Jupiter is the fifth planet from the Sun and the largest planet in the solar system. Its mass is 2.5 times that of all the other planets in the Solar System combined. Jupiter's diameter is 11 times larger and its volume is about 1,321 times larger than Earth's. Since Jupiter is less dense than Earth, Jupiter's mass is "only" 318 times larger than Earth's. If Jupiter could just somehow get 50 times more massive than it currently is, it could theoretically achieve stellar ignition and become a brown dwarf star. Alas, that is not in the cards, and so Jupiter remains a planet (gas giant).

Jupiter is thought to have a dense core surrounded by a layer of liquid hydrogen (and some helium) and an outer layer predominantly of gaseous hydrogen (and some helium), though much is still unknown. The temperature and pressure in Jupiter increases steadily as you approach its core. The temperature at the core-liquid hydrogen boundary is estimated to be 36,000 F and 2 million atmospheres (29 million psi)! Jupiter is covered with clouds of ammonia crystals. The clouds are arranged into bands at different latitudes. These bands sometimes will vary in width or color, but have remained a constant feature of Jupiter since first observed. More on these cloud bands found here.
Jupiter has a magnetic field that is 14 times stronger than the Earth's. This magnetic field is thought to be generated by eddy currents in the liquid hydrogen layer of Jupiter. It is the strongest in the solar system (except for those found in sun spots). The four largest moons of Jupiter all orbit within it's magnetic field and are protected by it against the solar wind.
Jupiter, on average, is 5.2 AU away from the sun and completes an orbit once every 11.86 years. The axial tilt of Jupiter is only 3.13° which is pretty small compared to Earth's 23.4°, so the gas planet doesn't really experience seasons. Jupiter rotates once every 10 hours making it the fastest rotating planet the the Solar System. Jupiter, when viewed from Earth, never has phases, since its orbit is outside of our own.
The Galilean Moons

Jupiter has 67 confirmed moons, but don't be intimidated, as you can see to the right, there are only 4 that really matter. They are, in order from largest to smallest, Ganymede, Callisto, Io, and Europa. These are referred to as the Galilean moons because they were discovered by Galileo Galilei in January of 1610. Galileo had recently made improvements to his telescope that allowed him to observe the moons. Of the Galilean moons, Io orbits the closest, next Europa, then Ganymede, and finally Callisto.
Io
Io, being so close to Jupiter at 422,000 km (about the Moon's distance from Earth), is the most geologically active object in the Solar System. Io has 400 active volcanoes, the result of tidal heating from Jupiter and the other Jovian Moons. Some of the volcanoes produce flumes up to 500 km (300 miles) above its surface. Io is primarily made of silicate rock surrounding a molten iron or iron sulfide core.
In 1979, Voyager I and II revealed Io to be a geologically active world with volcanoes, large mountains (some larger than Everest) and a young surface (no impact craters). Io takes 42.5 hours to complete one orbit around Jupiter. As with all the Galilean moons, Io rotates synchronously with its orbital period, keeping one face always pointed toward Jupiter. Io is slightly larger in volume than Earth's moon. It has a radius of 1,821 km (1,131 mi) and a mass of 9 x 1022 kg (21% larger than Earth's moon).

Europa
Europa is primarily made of silicate rock and probably has an iron core. It has a very thin atmosphere (10-12
times Earth's atmosphere) composed mostly of oxygen. It's surface is composed of
ice and is one of the smoothest in the Solar System. The surface is
covered by cracks and streaks. Surface craters are rare on the surface
of Europa. It is believed there is water under the ice surface and
Europa is a serious candidate for extraterrestrial life. The Hubble Space
Telescope has detected water vapor plumes (200 km high) on Europa
further strengthening the idea of an existing ocean under Europa's icy
crust.
Europa orbits Jupiter in just over three and a half days with an
orbital radius of about 670,900 km (Earth's moon is ~400,000 km). Europa is
3,100 km in diameter (slightly smaller than Earth's moon) and has a mass of 5
x 1022 kg (~2/3 mass of Earth's moon). Europa's surface temperature averages about 110 K (-160º C).
Ganymede
Ganymede is the largest moon in the Solar System with a radius of 5,268 km (Earth's radius is 12,742 km) and a mass of 1.5 x 1023 kg (2x the mass of the Earth's moon). Ganymede orbits Jupiter at a distance of 1,070,400 km. This is roughly three times the distance between the Earth and the Moon. Ganymede orbits Jupiter once every seven days and three hours.
Ganymede is thought to have an iron sulfide-iron core, silicate mantle and outer ice mantle. The surface of Ganymede consists of two types of terrain. Very old, highly cratered, dark regions that comprise one third of the surface and lighter regions with grooves and ridges covering the rest. The darker terrain contains clays and organic materials. The lighter terrain is thought to be composed of ice. It is speculated that there is an ocean of liquid water deep below the surface of Ganymede.
Callisto
The surface of Callisto is heavily cratered and very old. There are no signs of subsurface processes such as plate tectonics or volcanism. Callisto has an extremely thin atmosphere of carbon dioxide and a overall density that suggests Callisto is approximately equal parts rocky material and ice. It is speculated an ocean may exist under the crust. Beneath that ocean lies more rocky material. Callisto is not thought to contain a clearly defined core. The density of the rocky material just seems to gradually increase the closer to the center you get. Due to its stable surface, favorable orbit, and low surface radiation levels, Callisto has been identified as the likely location for a manned outpost to study Jupiter and its moons.
Callisto orbits Jupiter at a distances of 1,880,000 km (5x the distance between the Earth and the Moon). Callisto takes 16.7 days to orbit Jupiter. Callisto is the third largest moon in the Solar System, behind Ganymede and Titan. It has a diameter of 4820 km (Earth's = 12742 km) and a mass of 1.1 x1023 kg (1.5x more massive than Earth's moon).
Bonus Stuff
 
|
Comments rated to be Good Answers:
Comments rated to be "almost" Good Answers: