---
title: Ice giant
summary: A giant planet made mostly of water, methane and ammonia rather than hydrogen and helium, like Uranus and Neptune. Their interiors are hot, dense fluids, their magnetic fields are lopsided, and planets of about their mass may be among the commonest in the Galaxy.
science_status: [observed, model, sim]
categories: [Ice giants, Planet classes, Giant planets]
aliases: [Ice giants, IGC, IGH, IG1-C, IG2-H, Cold ice giant, Hot ice giant, Neptune-like planet, Uranus-like planet, Neptunian planet, Active ice giant, Quiescent ice giant, IGC-CA, IGC-CQ, IGH-WV, IGH-RB, IGH-DS, Water-veiled ice giant, Rayleigh-blue ice giant, Dark-stripped ice giant]
infobox:
  type: planet_class
  name: Ice giant
  image: File:Ice_giant_IGC-CQ_sim.png
  caption: "Sim render: the sim's quiescent, Uranus-like cold ice giant (IGC-CQ), a pale blue-green disc with gentle limb darkening"
  code: "IGC, IGH"
  legacy_code: "IG1-C, IG2-H"
  level: "Series (two sim types)"
  series: IG (ice giant)
  science_status: "observed (Uranus, Neptune); model (interiors); sim (subtypes)"
  literature_equivalent: "Ice giant; Neptune-mass planet ('Neptune-like')"
  defining_criteria: "Mostly elements heavier than hydrogen and helium by mass, with an H/He envelope of perhaps 10 to 20%. Sim: cold (IGC) split by internal heat into Active and Quiescent; hot (IGH) split by temperature, 350 to 700 K Water-Veiled, 700 to 1,200 K Rayleigh-Blue, above 1,200 K Dark-Stripped"
  mass: {value: "Uranus 14.5, Neptune 17.1; about 10 to 50 for the class", unit: M_Earth, source: observed, note: "Sim: 8 to 50 (cold), 6 to 50 (hot)"}
  radius: {value: "Uranus 25,559; Neptune 24,764 (about 4 Earth radii)", unit: km, source: observed}
  bulk_density: {value: "Uranus 1.27, Neptune 1.64", unit: g/cm³, source: observed}
  gravity_at_1_bar: {value: "Uranus 8.7, Neptune 11.0 (equatorial)", unit: m/s², source: observed}
  escape_velocity: {value: "Uranus 21.3, Neptune 23.5", unit: km/s, source: observed}
  temperature_at_1_bar: {value: "Uranus 76, Neptune 72", unit: K, source: observed}
  bond_albedo: {value: "Uranus 0.30, Neptune 0.29", unit: dimensionless, source: observed}
  dominant_gases: "H2 about 80%, He 15 to 19%, CH4 1.5 to 2.3% by volume in the upper atmosphere"
  cloud_and_haze_species: "Methane ice near 1 to 2 bar; hydrogen sulfide and haze below; NH4SH and water far deeper; photochemical haze above"
  wind_speeds: {value: "Neptune's equatorial winds about 400 westward; Uranus's jets up to about 250 eastward at mid-latitudes", unit: m/s, source: observed}
  magnetic_field: "Multipolar and offset: dipoles tilted about 59 (Uranus) and 47 (Neptune) degrees from the spin axis"
  interior_structure: "H/He envelope over a hot, electrically conducting fluid of water, ammonia and methane, possibly superionic at depth, over a rocky core; proportions uncertain"
  tidal_state: "Cold ice giants not locked (Uranus 17.2 h, Neptune 16.1 h); hot ones locked"
  typical_orbit: "Uranus 19.2 AU, Neptune 30.2 AU; Neptune-mass exoplanets from days to many AU"
  rings_moons: "Both have narrow dark rings and families of moons; Neptune's Triton is a captured body"
  frequency_in_sim: "752 of the 8,742 planets in the 5,159 generated systems (709 cold, 46 hot, including 3 legacy-coded bodies)"
  real_examples: "Uranus, Neptune; GJ 436 b (warm Neptune); LTT 9779 b (ultra-hot Neptune)"
  subtypes: "IGC-CA Active, IGC-CQ Quiescent; IGH-WV Water-Veiled, IGH-RB Rayleigh-Blue, IGH-DS Dark-Stripped (sim names)"
  sim_source: "Ice giant physics engine and properties module; the ice giant science reference"
  rendered_example: "IGC-CQ-AQ and IGC-CA-DP-1 (sim renders); 17 ice giant looks in the procedural generator"
  last_verified: "2026-09-27, writer B"
sim:
  entity: planet_series.IG
refs:
  - id: nasa_uranus
    type: webpage
    author: [{literal: "NASA Space Science Data Coordinated Archive"}]
    title: "Uranus Fact Sheet"
    URL: https://nssdc.gsfc.nasa.gov/planetary/factsheet/uranusfact.html
    accessed: 2026-09-27
  - id: nasa_neptune
    type: webpage
    author: [{literal: "NASA Space Science Data Coordinated Archive"}]
    title: "Neptune Fact Sheet"
    URL: https://nssdc.gsfc.nasa.gov/planetary/factsheet/neptunefact.html
    accessed: 2026-09-27
  - id: nasa_neptune_facts
    type: webpage
    author: [{literal: "NASA Science"}]
    title: "Neptune Facts"
    URL: https://science.nasa.gov/neptune/facts/
    accessed: 2026-09-27
  - id: helled2020
    type: article-journal
    author: [{family: Helled, given: Ravit}, {family: Fortney, given: Jonathan J.}]
    title: "The interiors of Uranus and Neptune: current understanding and open questions"
    container-title: "Philosophical Transactions of the Royal Society A"
    volume: 378
    page: 20190474
    issued: 2020
    DOI: 10.1098/rsta.2019.0474
  - id: millot2019
    type: article-journal
    author: [{family: Millot, given: Marius}, {family: Coppari, given: Federica}, {family: Rygg, given: J. Ryan}, {literal: "et al."}]
    title: "Nanosecond X-ray diffraction of shock-compressed superionic water ice"
    container-title: Nature
    volume: 569
    page: 251-255
    issued: 2019
    DOI: 10.1038/s41586-019-1114-6
  - id: pearl1991
    type: article-journal
    author: [{family: Pearl, given: J. C.}, {family: Conrath, given: B. J.}]
    title: "The albedo, effective temperature, and energy balance of Neptune, as determined from Voyager data"
    container-title: "Journal of Geophysical Research: Space Physics"
    volume: 96
    page: 18921-18930
    issued: 1991
    DOI: 10.1029/91JA01087
  - id: pearl1990
    type: article-journal
    author: [{family: Pearl, given: J. C.}, {family: Conrath, given: B. J.}, {family: Hanel, given: R. A.}, {literal: "et al."}]
    title: "The albedo, effective temperature, and energy balance of Uranus, as determined from Voyager IRIS data"
    container-title: Icarus
    volume: 84
    page: 12-28
    issued: 1990
    DOI: 10.1016/0019-1035(90)90155-3
  - id: wang2025
    type: article-journal
    author: [{family: Wang, given: Xinyue}, {family: Li, given: Liming}, {family: Roman, given: Michael}, {literal: "et al."}]
    title: "Internal Heat Flux and Energy Imbalance of Uranus"
    container-title: Geophysical Research Letters
    volume: 52
    page: e2025GL115660
    issued: 2025
    DOI: 10.1029/2025GL115660
  - id: irwin2022
    type: article-journal
    author: [{family: Irwin, given: P. G. J.}, {family: Teanby, given: N. A.}, {family: Fletcher, given: L. N.}, {literal: "et al."}]
    title: "Hazy Blue Worlds: A Holistic Aerosol Model for Uranus and Neptune, Including Dark Spots"
    container-title: "Journal of Geophysical Research: Planets"
    volume: 127
    page: e2022JE007189
    issued: 2022
    DOI: 10.1029/2022JE007189
  - id: irwin2024
    type: article-journal
    author: [{family: Irwin, given: Patrick G. J.}, {family: Dobinson, given: Jack}, {family: James, given: Arjuna}, {literal: "et al."}]
    title: "Modelling the seasonal cycle of Uranus's colour and magnitude, and comparison with Neptune"
    container-title: Monthly Notices of the Royal Astronomical Society
    volume: 527
    page: 11521-11538
    issued: 2024
    DOI: 10.1093/mnras/stad3761
  - id: limaye1991
    type: article-journal
    author: [{family: Limaye, given: Sanjay S.}, {family: Sromovsky, given: Lawrence A.}]
    title: "Winds of Neptune: Voyager observations of cloud motions"
    container-title: "Journal of Geophysical Research: Space Physics"
    volume: 96
    page: 18941-18960
    issued: 1991
    DOI: 10.1029/91JA01701
  - id: sromovsky2015
    type: article-journal
    author: [{family: Sromovsky, given: L. A.}, {family: de Pater, given: I.}, {family: Fry, given: P. M.}, {literal: "et al."}]
    title: "High S/N Keck and Gemini AO imaging of Uranus during 2012-2014: New cloud patterns, increasing activity, and improved wind measurements"
    container-title: Icarus
    volume: 258
    page: 192-223
    issued: 2015
    DOI: 10.1016/j.icarus.2015.05.029
  - id: hammel1995
    type: article-journal
    author: [{family: Hammel, given: H. B.}, {family: Lockwood, given: G. W.}, {family: Mills, given: J. R.}, {literal: "et al."}]
    title: "Hubble Space Telescope Imaging of Neptune's Cloud Structure in 1994"
    container-title: Science
    volume: 268
    page: 1740-1742
    issued: 1995
    DOI: 10.1126/science.268.5218.1740
  - id: ness1986
    type: article-journal
    author: [{family: Ness, given: Norman F.}, {family: Acuña, given: Mario H.}, {family: Behannon, given: Kenneth W.}, {literal: "et al."}]
    title: "Magnetic Fields at Uranus"
    container-title: Science
    volume: 233
    page: 85-89
    issued: 1986
    DOI: 10.1126/science.233.4759.85
  - id: ness1989
    type: article-journal
    author: [{family: Ness, given: Norman F.}, {family: Acuña, given: Mario H.}, {family: Burlaga, given: Leonard F.}, {literal: "et al."}]
    title: "Magnetic Fields at Neptune"
    container-title: Science
    volume: 246
    page: 1473-1478
    issued: 1989
    DOI: 10.1126/science.246.4936.1473
  - id: stanley2004
    type: article-journal
    author: [{family: Stanley, given: Sabine}, {family: Bloxham, given: Jeremy}]
    title: "Convective-region geometry as the cause of Uranus' and Neptune's unusual magnetic fields"
    container-title: Nature
    volume: 428
    page: 151-153
    issued: 2004
    DOI: 10.1038/nature02376
  - id: tsiganis2005
    type: article-journal
    author: [{family: Tsiganis, given: K.}, {family: Gomes, given: R.}, {family: Morbidelli, given: A.}, {family: Levison, given: H. F.}]
    title: "Origin of the orbital architecture of the giant planets of the Solar System"
    container-title: Nature
    volume: 435
    page: 459-461
    issued: 2005
    DOI: 10.1038/nature03539
  - id: suzuki2016
    type: article-journal
    author: [{family: Suzuki, given: D.}, {family: Bennett, given: D. P.}, {family: Sumi, given: T.}, {literal: "et al."}]
    title: "The Exoplanet Mass-Ratio Function from the MOA-II Survey: Discovery of a Break and Likely Peak at a Neptune Mass"
    container-title: The Astrophysical Journal
    volume: 833
    page: 145
    issued: 2016
    DOI: 10.3847/1538-4357/833/2/145
  - id: mazeh2016
    type: article-journal
    author: [{family: Mazeh, given: T.}, {family: Holczer, given: T.}, {family: Faigler, given: S.}]
    title: "Dearth of short-period Neptunian exoplanets: A desert in period-mass and period-radius planes"
    container-title: Astronomy & Astrophysics
    volume: 589
    page: A75
    issued: 2016
    DOI: 10.1051/0004-6361/201528065
  - id: ehrenreich2015
    type: article-journal
    author: [{family: Ehrenreich, given: David}, {family: Bourrier, given: Vincent}, {family: Wheatley, given: Peter J.}, {literal: "et al."}]
    title: "A giant comet-like cloud of hydrogen escaping the warm Neptune-mass exoplanet GJ 436b"
    container-title: Nature
    volume: 522
    page: 459-461
    issued: 2015
    DOI: 10.1038/nature14501
  - id: hoyer2023
    type: article-journal
    author: [{family: Hoyer, given: S.}, {family: Jenkins, given: J. S.}, {family: Parmentier, given: V.}, {literal: "et al."}]
    title: "The extremely high albedo of LTT 9779 b revealed by CHEOPS"
    container-title: Astronomy & Astrophysics
    volume: 675
    page: A81
    issued: 2023
    DOI: 10.1051/0004-6361/202346117
images_wanted:
  - file: File:Ice_giant_IGC-CQ_sim.png
    subject: "The sim's quiescent (Uranus-like) cold ice giant: a pale blue-green, almost featureless disc darkening gently toward the limb"
    source: sim
    source_ref: "QA:gas_giant_limb_policy_stage_capped/aq_four_radii_sun20.png"
    credit: "Pax Abyssi (sim render, in-game look-development stage)"
    note: "1600 x 900 stage frame, no HUD."
  - file: File:Ice_giant_IGC-CA_sim.png
    subject: "The sim's active (Neptune-like) cold ice giant as a gibbous disc, deep blue with a bright streak of high cloud"
    source: sim
    source_ref: "QA:gas_giant_limb_policy_stage_capped/dp_four_radii_sun70.png"
    credit: "Pax Abyssi (sim render, in-game look-development stage)"
    note: "Caption must say the palette is bluer than Neptune's true colour (Irwin et al. 2024)."
  - file: File:Neptune_Webb_NIRCam_weic2214c.jpg
    subject: "Webb near-infrared image of Neptune with its rings and bright high-altitude methane-ice clouds"
    source: esa-webb
    page_url: https://esawebb.org/images/weic2214c/
    credit: "NASA, ESA, CSA, and STScI"
    licence: "CC BY 4.0 (ESA/Webb usage terms)"
---

An **ice giant** is a giant planet made mostly of elements heavier than hydrogen and helium: chiefly water, methane and ammonia, which planetary scientists call "ices" whatever their state. Uranus and Neptune are the two in the Solar System, each about 15 to 17 times Earth's mass and four times its width. Despite the name, almost nothing inside them is frozen: most of each planet is a hot, dense, electrically conducting fluid under a comparatively thin hydrogen-helium atmosphere :cite[helled2020]. Planets of about Neptune's mass appear to be among the most common in the Galaxy, which makes the two least-explored planets of the Solar System templates for a very large class.

## Characteristics

### Built differently from Jupiter

Jupiter and Saturn are mostly hydrogen and helium. Uranus and Neptune are not: at least 80% of Neptune's mass is a hot, dense fluid of water, methane and ammonia :cite[nasa_neptune_facts]. Their densities, 1.27 g/cm³ for Uranus and 1.64 for Neptune :cite[nasa_uranus] :cite[nasa_neptune], sit between those of the gas giants and the rocky planets. Their interiors are usually modelled as three layers: a hydrogen-helium envelope, a deep "mantle" of water-rich fluid, and a rocky core. The proportions are uncertain, because the same gravity field can be matched by different mixtures of rock and water, and the boundaries between layers may be gradual rather than sharp :cite[helled2020].

The pressures in an ice giant never become high enough in its thin hydrogen envelope to make metallic hydrogen, so the magnetic field must come from somewhere else. At the millions of atmospheres and thousands of degrees of the deep mantle, water is ionic and conducts electricity. Laboratory shock experiments have produced **superionic** water ice under such conditions: a crystal lattice of oxygen through which hydrogen ions flow like a liquid :cite[millot2019].

### Tilted, lopsided magnetic fields

Voyager 2, the only spacecraft to visit either planet, found magnetic fields unlike any other planet's. Uranus's dipole is tilted about 59 degrees from its spin axis and offset from the centre by about a third of the planet's radius :cite[ness1986]; Neptune's is tilted about 47 degrees and offset by more than half its radius :cite[ness1989]. Both fields also have strong components more complex than a simple dipole. Models reproduce this if the field is generated in a thin convecting shell of conducting fluid above a stable interior, rather than in a deep, fully convecting region :cite[stanley2004].

### Hot Neptune, cold Uranus

The two planets are near twins in size and mass but not in heat. Neptune radiates about 2.6 times as much energy as it absorbs from the Sun :cite[pearl1991]. Voyager found Uranus's output almost indistinguishable from the sunlight it absorbs :cite[pearl1990]; a 2025 reanalysis of Uranus's reflected light finds that it emits about 12.5% more than it absorbs, a small but real internal heat flow :cite[wang2025]. Why Uranus holds its heat in is unresolved; suggestions include a giant impact, which may also explain its 98-degree tilt, and layers in the interior that block convection :cite[helled2020].

### Clouds, colour and wind

The top clouds of an ice giant are methane ice, near 1 to 2 bar, with a thicker layer of haze and hydrogen sulfide ice below :cite[irwin2022]. Methane gas absorbs red light, which is why both planets are blue-green. Their true colours are more alike than the familiar Voyager images suggest. Both are a pale greenish blue; Neptune is only slightly bluer, because Uranus has a thicker layer of haze over its methane cloud. Voyager's images of Neptune were contrast-stretched to bring out its clouds, which made it look a much deeper blue than it is :cite[irwin2024].

Neptune, the planet farthest from the Sun, has the fastest winds measured on any planet: Voyager tracked clouds moving westward at about 400 m/s near the equator :cite[limaye1991]. Uranus's winds are gentler, with eastward jets near 60 degrees latitude of about 250 m/s :cite[sromovsky2015]. Neptune also makes large dark storms. The Great Dark Spot that Voyager photographed in 1989, about the size of Earth, was gone when the Hubble Space Telescope looked in 1994 :cite[hammel1995]; new spots have appeared and faded since, each lasting a few years.

::figure{src="File:Neptune_Webb_NIRCam_weic2214c.jpg" size=wide alt="Neptune in near-infrared light, a dim disc ringed by thin bright rings, with bright clouds in its southern hemisphere" caption="Observation: Neptune and its rings in near-infrared light from the James Webb Space Telescope, 2022. The planet looks dark because methane absorbs these wavelengths; the bright patches are high methane-ice clouds. Credit: NASA, ESA, CSA, and STScI."}

## Formation

Ice giants are a puzzle for formation models. At 20 to 30 AU from the Sun, solid material was sparse and orbits slow, so growing a core of more than ten Earth masses before the gas disc disappeared would have taken too long. One answer is that Uranus and Neptune formed closer to the Sun and were pushed outward later, when the orbits of the giant planets were rearranged; the Nice model reproduces the giants' present orbits this way :cite[tsiganis2005]. Their modest hydrogen-helium envelopes suggest that their cores reached the size for runaway gas capture only as the disc was fading, so they never became gas giants.

## Neptune-like planets around other stars

Microlensing surveys, which can detect planets several AU from their stars, find that planets of about Neptune's mass-to-star ratio are the most common type in that region :cite[suzuki2016]. Close to their stars, however, Neptune-sized planets are rare: there is a **hot Neptune desert** at orbital periods shorter than two to four days, probably because such planets lose their atmospheres to starlight or never arrive there :cite[mazeh2016]. The warm Neptune GJ 436 b trails a comet-like cloud of escaping hydrogen that blocks 56% of its star's ultraviolet light in transit, against 0.7% of visible light for the planet itself :cite[ehrenreich2015]. LTT 9779 b, an ultra-hot Neptune inside the desert, is unexpectedly reflective, with a geometric albedo of about 0.8, similar to Venus's, best explained by silicate clouds in a very metal-rich atmosphere :cite[hoyer2023]. Whether such planets have ice-giant interiors like Uranus and Neptune, or rocky cores with thick envelopes, usually cannot be told from mass and radius alone; the smaller, commoner [[Mini-Neptune|mini-Neptunes]] are a separate class.

## How we know

Voyager 2 flew past Uranus in 1986 and Neptune in 1989, and everything known about their magnetic fields, interiors and moons at close range comes from those two passes. Since then the Hubble Space Telescope, large ground-based telescopes with adaptive optics and JWST have tracked their clouds, storms, seasons and rings. Neptune-mass exoplanets are found by transits, radial velocities and microlensing.

## Notable examples

| Planet | Mass | Radius | Orbit | Notes |
|---|---|---|---|---|
| Uranus | 14.5 Earth masses | 25,559 km | 19.2 AU, 84 years | Tilted 97.8 degrees; little internal heat :cite[nasa_uranus] :cite[wang2025] |
| Neptune | 17.1 Earth masses | 24,764 km | 30.2 AU, 165 years | Fastest winds; emits 2.6 times what it absorbs :cite[nasa_neptune] :cite[pearl1991] |
| GJ 436 b | about 22 Earth masses | about 4 Earth radii | 2.6 days | Warm Neptune losing hydrogen :cite[ehrenreich2015] |
| LTT 9779 b | about 29 Earth masses | about 4.7 Earth radii | 0.8 days | Ultra-hot Neptune with an albedo near 0.8 :cite[hoyer2023] |

::figure{src="File:Ice_giant_IGC-CA_sim.png" size=wide alt="A deep blue planet seen gibbous, with a thin bright white cloud streak near its limb" caption="Sim render: the sim's active, Neptune-like ice giant. Its deep blue is the game's palette, bluer than Neptune's true pale greenish blue."}

:::callout{type=sim title="In Pax Abyssi"}
The sim has cold ice giants (IGC) and hot ice giants (IGH). Cold ice giants are split by internal heat, following the Uranus and Neptune pair: **Active** (IGC-CA, Neptune-like, emitting two to three times the sunlight it absorbs, with fast westward equatorial jets, thin haze and a chance of a dark spot) and **Quiescent** (IGC-CQ, Uranus-like, little internal heat, slower winds and thicker haze). Hot ice giants, for Neptune-mass planets closer to their stars, take names of the sim's own by temperature: **Water-Veiled** (350 to 700 K), **Rayleigh-Blue**, a cloudless blue planet (700 to 1,200 K), and **Dark-Stripped** (above 1,200 K). There are 752 ice giants among the 8,742 planets of the 5,159 generated systems, 709 of them cold.

The procedural gas giant generator (BUILT, awaiting the owner's verdict) has 17 ice giant looks. It gives ice giants a westward equatorial jet, softer limb darkening and a pale haze at the limb. One of the first flyable stops takes the ship to a Neptune-class ice giant generated for Xi Bootis, a real Sun-like star 22 light years away.
:::

## See also

- [[Gas giant]]
- [[Mini-Neptune]]
- [[Hot Neptune desert]]
- [[Exotic worlds]]
- [[Planetary rings]]
- [[Sol]]
