Jovian planets: Jupiter, Saturn, Uranus, and Neptune.
Detailed knowledge primarily gained from spacecraft rather than ground-based telescopes.
Importance of various missions to explore these planets.
Voyager Missions (1970s)
Voyager 1: Explored Jupiter and Saturn.
Voyager 2: Explored Saturn, Uranus, and Neptune.
Conducted studies on electromagnetic (EM) fields and used different fields of light (radio, visible, infrared).
Returned valuable data for analysis.
GALILEO Mission
Launched in the late 1980s, arrived at Jupiter in the mid-1990s.
Equipped with an atmospheric sensor to study Jupiter's atmosphere and its moons (detailed in Chapter 8).
Cassini Mission
Launched in the late 1990s, focused on Saturn and its moon Titan.
Continues to operate, studying the planet, rings, and moons.
Size and Mass Comparison
Jovian planets are significantly larger and more massive than Earth.
Earth as a baseline: mass = 1, radius = 1.
Other Jovian planets have masses many times greater than Earth.
Surface Gravity and Density
Surface gravity much greater for Jupiter, Saturn, Uranus, and Neptune compared to Earth.
All have lower average densities (~1000 kg/m³), with Saturn being less dense than water, theoretically capable of floating.
Predominantly composed of hydrogen and helium.
Low-density nature due to massive gravitational force retaining atmospheric gases:
Unlike terrestrial planets that lost their original atmospheres, Jovian planets maintained them through stronger gravity.
Core Structure
Possibly a rocky or icy core beneath atmospheric layers.
Electromagnetic Fields
Generated by the rotation of the mantle.
Emit radio waves, contributing to their electromagnetic signature.
Rotation varies by planet, with different inclinations:
Jupiter: nearly straight up and down.
Saturn: tilted at about 26-27 degrees.
Uranus: tipped on its side (97 degrees).
Neptune: tilted at about 30 degrees.
Differential Rotation
Parts of the planet rotate at different speeds:
Jupiter's high latitudes take longer (six minutes) compared to the equator.
Saturn has a 25-minute difference.
Uranus has a two-hour difference; Neptune has a six-hour difference.
No solid surface; core and mantle models based on physical and chemical data:
Core potentially rocky or icy, specially in Uranus and Neptune.
Mantle primarily consists of compressed hydrogen:
Exhibits a slushy or metallic characteristic, indicating high pressure.
Atmosphere constitutes the outer layer, with no defined crust.
The next mission aims to delve deeper into understanding Jovian planets through animated models.
Focus on comparative sizes, internal structures, and the excess heat radiation emitted by Jupiter and Saturn, suggesting significant internal energy.