Gas Giant Magnetic Field Extreme Activity
Why is this a Gas Giant? Your planet has 85.0% hydrogen and helium, combined with a mass of 95.0x Earth, which exceeds the gas giant threshold. Gas giants form when massive cores capture enormous atmospheres of light gases. They typically form beyond the 'frost line' where volatiles can condense.
✓ Hydrogen + Helium: 85.0% (>60% required) ✓ Mass: 95.0x Earth (>10x required)
Habitability Score Marginal
Contributing Factors water 15
No solid surface — any water is locked in a supercritical mantle and hot ice, not oceans geology 50
Extreme volcanic activity may be hazardous (tidal flexing sustains geologic activity) rotation 10
Near tidally locked - one hemisphere perpetually scorched, other frozen, narrow habitable twilight zone only Organic Chemistry 80
Core organic elements (CHNO) present atmosphere 12
Hydrogen-rich atmosphere typical of gas giants (partially stripped by slow rotation) temperature 40
Extreme temperature - very difficult for life magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
95.00x Earth (5.67e+26 kg) Radius
4.56x Earth (29,070 km) This planet: 4.56× Earth radius Earth: 1× (baseline)
Surface Gravity
4.56x Earth (44.8 m/s²) Surface Temperature
202 K (-71 °C / -95 °F) Rotation Period
11.0 hours/day (faster than Earth) This planet: 11 h/day Earth: 24 h/day Orbital Environment Star Type
A-type (Blue-White) Distance from Star
12.20 AU (1.83 billion km) Atmosphere Hydrogen and helium dominated with trace methane and ammonia
Surface Characteristics No solid surface - thick gaseous envelope with possible rocky core deep within Moons
Moon 1 receding Ocean world 0.089% - 5.9 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
A thin tidal-warmed subsurface ocean may exist, but conditions are marginal (16/100).
Moon 2 receding Ocean world 0.13% - 15.4 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
A thin tidal-warmed subsurface ocean may exist, but conditions are marginal (7/100).
+10 geology: tidal flexing sustains geologic activity