Jupiter Module 5
Module 5: Jupiter
Observations of Jupiter from Earth
Visibility: Third brightest object in night sky.
Size: Largest planet in the solar system.
Telescope Observations:
Simple telescopes can reveal moons and alternating color patterns.
Notable features include bands and ovals.
Moons: Jupiter has many moons.
Galilean Moons: Name given to its four largest moons.
Jupiter's Atmosphere – Two Main Features
Cloud Bands:
Features numerous parallel cloud bands of varying colors (yellow, blue, brown, tan, red).
The Great Red Spot:
A massive, hurricane-like storm that is three times the size of Earth.
Has persisted for hundreds of years.
Jupiter's Atmosphere – Composition
Composition:
Hydrogen: 86% (most abundant)
Helium: 14%
Other gases: Methane, ammonia, water vapor.
Coloration:
No single gas is responsible for the planet's colors.
Colors are due to chemical processes occurring in a turbulent atmosphere.
Trace gases such as sulfur and phosphorous contribute reds, browns, and yellows.
Energy Sources: Internal heat drives energy for these reactions; the magnetosphere and lightning also play a role.
Jupiter's Atmosphere - Bands
Light and Dark Bands:
These bands vary with latitude and intensity but are always present.
Explored by space probes Voyager and Cassini.
Convection Mechanism:
Zones: Areas of upward motion.
Belts: Areas of sinking air.
Jupiter's Atmosphere
Belts & Zones:
Pressure areas control weather patterns.
Bands wrap around the planet with cloud formation at different heights.
Temperature differences affect cloud chemistry, resulting in varied colors.
Jupiter's Atmosphere – Jet Stream
Stable Zonal Flow:
Features east-west flow mainly at the equator, termed the easterly jet stream.
Poles exhibit a slow, steady flow without distinct bands.
Layers of Jupiter's Atmosphere
Troposphere: The uppermost layer with distinct colored cloud layers below.
Convection: Controls cloud distribution.
Haze Layer: Found above the troposphere.
Clouds Composition:
Ammonia Ice Clouds: Up to 30km high with temperatures between 125-150 K.
Ammonium Hydrosulfide Ice Clouds: Found below ammonia clouds at around 200 K.
Water Vapor & Ice Clouds: Located 80 km beneath the troposphere top.
Galileo Atmospheric Probe Observations
Key Measurements: Wind speed, temperature, composition confirmed theoretical models.
Altitude Observations: 0 km to 200 km.
Stratosphere and Troposphere: Information on pressure and temperature profiles across atmospheric layers.
Jupiter's Weather
Great Red Spot:
Active for over 300 years, it resembles a hurricane and has been studied by Voyager and Galileo missions.
Persistent and large, spans about 25,000 km and engulfs smaller storms while rotating with Jupiter's interior.
Jupiter’s Weather – Zonal Flow
Movement:
Northward motion is west, while southward is east.
Exhibits turbulent eddies with calmer centers.
Voyager Discoveries: Identified smaller storms, including white ovals (high cloud tops) and brown ovals.
In 2006, a spot changed from white to brown to red, indicating a strong storm that lifted clouds underneath due to UV radiation-induced chemical reactions.
Jupiter’s Weather – Small Storms
Similar color changes have been observed in smaller storms, with the red color indicating a strong storm activity due to the same UV radiation reactions.
Jupiter’s Interior
Temperature & Pressure: Increase steadily with depth; stratified into gas and liquid layers.
Hydrogen Mantle: Exists in a metallic state, behaving like a liquid metal, which helps conduct heat and forms Jupiter's magnetic field.
Jupiter’s Interior - Core
Core Characteristics:
Bulging at the equator, indicating a more complex structure than just hydrogen and helium.
Dense core possibly composed of molten or semi-solid rock with iron, with a diameter of about 20,000 km.
Magnetosphere
Magnetic Field Strength: A strong magnetic field, produced by rapid rotation and electrically conductive fluids.
Size: 20,000 times stronger than Earth’s, with an uneven structure:
Sun-side extends approximately 3 million km, while the opposite side reaches up to 600 million km.
Overall magnetosphere spans 30 million km, exceeding the size of the sun.
Aurorae
Occurrence: Similar to Earth's auroras, caused by charged solar wind particles being deflected into Jupiter’s atmosphere by its magnetic field.
Internal Heating
Temperature Insights: Originally thought to be around 105 K; actual measurement reveals it to be approximately 125 K.
Heat Source: Results from residual heat from formation; the interior used to be hotter than it currently is, and heat leaks drive storm formation, being trapped by cloud layers.