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Entering orbit…
Habitability
0/ 100
Uninhabitable
CFHTWIR-Oph 98 b rendered in TerraForge from its measured mass, orbit and star

CFHTWIR-Oph 98 b

Also written CFHTWIR-Oph 98b, CFHTWIR Oph 98b, CFHTWIR Oph 98 b

Gas GiantFound 2020
Mass
2480.00 × Earth
Radius
20.80 × Earth
Gravity
5.73 g
Surface (est.)
4 K
Year
22,012 years
Day (est.)
24.0 hrs
Mass
2480.00 × Earth
Radius
20.80 × Earth
Gravity
5.73 g
Surface (est.)
4 K
Year
22,012 years
Day (est.)
24.0 hrs

CFHTWIR-Oph 98 A system

Type
M-type (Red Dwarf)
Spectral type
M9-L1
Temperature
2,320 K
Radius
0.245 ☉
Mass
0.0147 ☉
Planets
1
Luminosity
1.41e-3 ☉

Published by the NASA Exoplanet Archive. This world’s temperature and habitability score are computed from this star’s measured luminosity, not from a stand-in for its class.

CFHTWIR-Oph 98 b200.00 AUYou are here2,480 M⊕
Habitable zone

Star and planets drawn to scale: the star is 1.3 times as wide as CFHTWIR-Oph 98 b, so only its edge is in view. Orbits spaced as in the star system view.

Estimated: this planet doesn't transit its star, so its size is inferred, not measured

CFHTWIR-Oph 98 b, from the NASA Exoplanet Archive (found 2020). Measured: 2480 Earth masses, 200 AU, a 2320 K M-type star. Composition inferred from a mass of 2480 Earths, which is giant territory whatever its 0.28x density suggests, with an assumed 24-hour day — rotation cannot be measured for exoplanets. Note: TerraForge comes out at 4 K against the archive's 1800 K, because that figure is the planet's own heat, not the star's. It receives almost no sunlight out at this distance and is still glowing from its formation — TerraForge only warms worlds with starlight, so it has no way to model a planet heated from within.

Surface. No solid surface - thick gaseous envelope with possible rocky core deep within

Gas Giant
Magnetic FieldExtreme Activity
CFHTWIR-Oph 98 b has 86.0% hydrogen and helium, combined with a mass of 2480.0x 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.
Classification Criteria:
✓ Hydrogen + Helium: 86.0% (>60% required)✓ Mass: 2480.0x Earth (>10x required)

Reading CFHTWIR-Oph 98 b’s atmosphere

Dominant elements: H, He, O, C, NThis is what a telescope would measure while CFHTWIR-Oph 98 b crosses in front of its star: starlight passes through the atmosphere and spreads into a rainbow band. Each dark line marks a wavelength the atmosphere absorbed.Every element absorbs its own signature wavelengths — hydrogen always darkens the same two spots, calcium another pair, and so on. Astronomers match the lines in a real spectrum against a library of these signatures to say what an atmosphere is made of, light-years away, without ever visiting. A deeper line generally means more of that element is present.For a real planet, distance is usually measured by parallax: as Earth orbits the Sun, a nearby star appears to shift very slightly against the distant background stars, and the size of that shift gives its distance directly — the same geometry surveyors use, at an interstellar scale.
Further reading
ExoplanetsSara Seager (editor)The field's standard reference: how planets are found, how they form, and what their atmospheres are made of.The Planet FactoryElizabeth TaskerHow planets are made, and why so few of them come out like Earth.Exoplanets: Diamond Worlds, Super Earths, Pulsar PlanetsMichael Summers & James TrefilThe strange end of the catalogue — carbon worlds, molten rock, planets orbiting dead stars.The Little Book of ExoplanetsJoshua WinnHow these worlds are found, and what a measurement can honestly tell us.
As an Amazon Associate I earn from qualifying purchases — if you buy through these links, TerraForge may receive a small commission at no extra cost to you.
Habitability ScoreUninhabitable
0
Contributing Factors
temperature0
Near absolute zero - all molecular activity ceases, impossible for life
atmosphere30

Hydrogen and helium dominated with trace methane and ammonia

Hydrogen-rich atmosphere typical of gas giants
water15
No solid surface — any water is locked in a supercritical mantle and hot ice, not oceans
magnetic Field100
Magnetic field provides radiation protection
geology40
Extreme volcanic activity may be hazardous
Organic Chemistry80
Core organic elements (CHNO) present
rotation100
Optimal rotation period - balanced day/night cycle, moderate weather, and good heat distribution

Physical Properties

Mass
2480.00x Earth (1.48e+28 kg)
Radius
13.54x Earth (86,237 km)
This planet: 13.54× Earth radiusEarth: 1× (baseline)
Surface Gravity
13.54x Earth (132.8 m/s²)
Surface Temperature
4 K (-269 °C / -453 °F)
Rotation Period
24.0 hours/day
This planet: 24 h/dayEarth: 24 h/day

Elemental Composition

A dark ringed planet hanging over the horizon of a rocky moon, its rings lit by a distant sun

New: Stand on Your Moons 🌒

A planet's surface view isn't the only ground any more. Press the surface button on a planet with moons and it asks where to stand: the planet itself, or any moon still in orbit, each tagged with what it became — ocean, ice, carbon, volcanic. Every moon gets its own ground and sky from its own physics: airless rock under a black sky, ice cracked by geysers over a hidden sea, sulfur plains shaking with eruptions, or orange haze you can't see the sun through. And hanging over the horizon, there's the planet you built.

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