Gas Giant Magnetic Field Extreme Activity
Why is this a Gas Giant? Your planet has 71.5% hydrogen and helium, combined with a mass of 11.0x 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: 71.5% (>60% required) ✓ Mass: 11.0x Earth (>10x required)
Habitability Score Uninhabitable
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 84
Core organic elements (CHNO) present (tidal pools cycle wet and dry - a boost for prebiotic chemistry) atmosphere 12
Hydrogen-rich atmosphere typical of gas giants (partially stripped by slow rotation) temperature 25
Very cold - water frozen, challenging for life (large moon stabilizes the axial tilt - steady seasons) magnetic Field 100
Magnetic field provides radiation protection Physical Properties Mass
11.00x Earth (6.57e+25 kg) Radius
2.22x Earth (14,169 km) This planet: 2.22× Earth radius Earth: 1× (baseline)
Surface Gravity
2.22x Earth (21.8 m/s²) Surface Temperature
100 K (-173 °C / -279 °F) Rotation Period
8.0 hours/day (faster than Earth) This planet: 8 h/day Earth: 24 h/day Orbital Environment Star Type
G-type (Yellow (Sun-like)) Distance from Star
7.69 AU (1.15 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 Life may exist on a moon
Moon 1 receding Ocean world - life 0.079% - 10.3 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Tidal braking locked the planet to its moon: one face forever moonward.
Tidal heat sustains a subsurface ocean over a rock seafloor: a strong candidate for life (Europa-like, 50/100).
Moon 2 stable 0.022% - 18.2 radii
Small and distant: a quiet, stable companion.
Moon 3 receding 0.056% - 37.0 radii
Outside the synchronous orbit: slowly receding, like Luna (~cm per year).
Moon 4 stable Ocean world 0.013% - 4.6 radii
Small and distant: a quiet, stable companion.
A thin tidal-warmed subsurface ocean may exist, but conditions are marginal (28/100).
Moon 5 merged 1.0% - 53.8 radii
Merged with an adjacent moon: too close for both to hold a stable orbit.
+5 temperature: large moon stabilizes the axial tilt - steady seasons +10 geology: tidal flexing sustains geologic activity +4 chemistry: tidal pools cycle wet and dry - a boost for prebiotic chemistry