Rings of the Jovian Planets Module 5
Module 5
Rings of the Jovian Planets
All four Jovian planets have rings.
Materials in the rings consist of tiny particles to small "moonlets."
Formation theories:
May form when a moon(s) is destroyed.
Composed of material that couldn’t form a moon.
Strong gravity of the Jovian planets allow large bodies to be torn apart by tidal forces, resulting in smaller particles remaining intact.
Discovery of Saturn’s Rings
1610: Galileo observes Saturn with "ears."
1655: Christaan Huygens posits that Saturn is surrounded by a solid ring.
1676: Giovanni Cassini discovers a gap in the rings, named the Cassini Division.
The main rings extend from 7,000 km to 80,000 km (4200-48000 miles) above Saturn's equator, with a thickness of only 10 meters (32 feet).
Composed of 99.9% pure water ice.
Ring particles vary in size from 1 cm to 10 m.
Saturn’s Rings
Visible from Earth: Three main rings – A, B, C
Ring A: Farthest; second brightest
Ring B: Brightest
Ring C: Translucent, closest to the planet
Small Encke gap in A ring and Cassini Division (dark gap) present.
Rings D-F not visible from Earth.
Formation of Saturn’s Rings
Characteristics: Rings may be relatively young, potentially only 50 million years old.
Factors influencing formation:
Waves, collisions, or interactions with moons can create and replenish ring material.
Recent catastrophic events could lead to moons being torn apart by gravity or impacts.
Example: Saturn's ring mass could result from a 250 km diameter satellite.
Triton, a moon of Saturn, is expected to eventually create a ring system.
Saturn’s Rings – Variations by Season
Seasonal changes occur due to Saturn's tilted axis and orbit.
Brightness of rings changes with axial tilt:
North/South pole towards the sun: Bright appearance.
Spring and fall: Rings appear edge-on, becoming hard to see.
Changing Aspects of Saturn's Rings
Changes observed as Earth and Saturn orbit the Sun, which takes 29.457 Earth years.
Images from the Hubble Space Telescope show Saturn's appearance changes.
Roche Limit
How rings form:
A small moon approaches Saturn and becomes stretched by gravity tidal forces until it’s torn apart.
Pieces spread into individual orbits, forming rings.
Roche limit: Minimum distance from a planet where a space object will be torn apart.
Approximately 2.4 times the planet radius.
Not applicable to smaller space objects held together by interatomic/electromagnetic forces rather than gravity.
Details of Saturn’s Rings
Voyager 2: Discovered main rings contain tens of thousands of ringlets.
Ringlet characteristics:
Ring particles come together and disperse; contain narrow gaps.
Presence of moonlets (10-20 km across) which impact particles.
Cassini Division
Caused by the gravity of the moon Mimas, which deflects ring particles into new orbits, clearing the division.
F-ring
Discovered by Pioneer 11 in 1979.
Appears as a braided strand and is thin.
Is maintained by shepherd satellites, such as Pandora.
D-ring
Faint and located inside the C-ring, closer to cloud tops.
Contains few dark particles, making it invisible from Earth.
E-ring
Located outside the main rings, comprised of diffuse dust.
Discovery of Jupiter’s Rings
Voyager found a faint ring around Jupiter, located inside the inner moon orbit.
Consists of dark rock fragments and dust, resulting from chipped-up moons by meteorites.
The ring is thin, measuring only several tens of kilometers thick.
Jupiter's Rings
Rings are faint and challenging to see.
Enhanced images display a gossamer appearance composed of:
Main Ring
Halo
Amalthea, Adrastea, Metis, Thebe
Uranus's Ring System
First discovered in 1977; it has 11 thin rings.
The rings are dark, narrow, and widely spaced, exhibiting a very thin structure.
Neptune’s Rings
Comprises four dark rings, including three that are narrow and one broad/diffuse ring.
The outer rings exhibit clumping; some areas are too thin.
Clumping may be attributed to shepherd satellites.