Planet Sunsets

At sunset on Mars, the glow around the Sun is blue. Drag down to set the Sun, drag sideways to travel from Venus out to Uranus: each world has its own air, its own distance from the Sun, its own light.

    Drag the picture up or down for the sunset, left or right for your distance from the Sun. The arrow keys do the same.

    Seven skies, the Sun at the same point

      Tap a frame to change world. In every frame the Sun has gone the same way towards setting, measured against that world’s own sunset.

      About this tool

      Three layers make up the picture, and the label on it names them. The sky’s colours come from tables sampled from NASA’s simulated video (NASA Goddard SVS 13645, by Geronimo Villanueva and James Tralie, made with the Planetary Spectrum Generator). The ground on Mars, Venus and Titan is an AI-imagined picture, generated from a text description: it is not a photograph and shows no real place. The Sun, its glow, the sea and Uranus’s clouds are this page’s own drawing. No spacecraft photograph is shown on this page.

      Why are Martian sunsets blue? From JPL’s caption of Curiosity’s photograph: fine dust lets blue light through more efficiently, so blue stays close to the Sun while yellow and red scatter more widely, and the effect is strongest at sunset because the light path is longest. The colour table taken from NASA’s video runs from tan to a white that clips near the Sun, so on Mars, from mid-dusk on, this page changes the hue: the brightness is still the simulation’s, but the colour follows the pattern measured in that photograph, blue-white near the Sun and fading to grey-blue. This is an adjustment made here, not NASA’s output; the link above shows the real thing.

      Not every world is hazy, so the air over the land is set per world. Mars: about 0.006 bar, 95% carbon dioxide, thin air with fine dust, so distant ridges stay clear. Venus: 92 bar, 96.5% carbon dioxide, with sulfuric-acid cloud hiding the Sun from far overhead, not fog on the ground; but air that dense scatters strongly by itself (roughly a kilometre’s mean free path in green light), so distant land fades there too. Titan: about 1.5 bar, about 95% nitrogen and 5% methane, in orange haze that softens distant land (Huygens’s data imply the air near the ground was clear for tens of kilometres). Earth’s three skies show clear air, haze and overcast over a drawn sea. Uranus is 82.5% hydrogen and 15% helium, with no ground at all. Distance sets the Sun’s size, from 1.38× Earth’s at Venus to 0.052× at Uranus.

      What up and down means: NASA’s simulation never states where the Sun is, so dragging up and down moves through its frames, and the percentage is how far the Sun has gone towards this page’s estimate of that world’s sunset, not degrees of elevation. The Sun’s height and the picture’s brightness are schematic: Titan’s real surface in particular is far darker than this, and Venus’s is dimmer and more orange. On Mars the glow is also moved to surround the Sun, which the table does not do. Venus and Titan show no crisp Sun, only a diffuse glow, and Earth under overcast shows the same. Uranus’s clouds are schematic, drawn from the table’s own colours.

      Dragging left or right moves along the distance from the Sun. Between two stops the page fades one world into the other under a single Sun whose size follows the distance, though only Earth, Mars and Uranus show one to see, since Venus and Titan have only a glow. The blend is a transition, not a simulated atmosphere, and the label says so while it lasts. What travels with you, and what the strip and the percentage show, is how far the Sun has gone towards setting on each world, so a set Sun stays set and coming back returns the same moment. Each world’s sunset point is this page’s estimate from its colour table (where the glow at the horizon starts to fall), not a figure from NASA. The shared clock runs every Sun through sinking its own diameter, the one span this page has a real time for; NASA’s simulation has no time axis, so the rest of the dusk has none.

      How the numbers are computed, in one function: the Sun’s apparent diameter is 0.5332° divided by the mean distance in AU (Venus 0.723, Earth 1, Mars 1.524, Titan 9.58, Uranus 19.19); the time to sink its own diameter is that diameter ÷ 360° × the length of the solar day, at the equator at equinox (Venus 116.75 days, Earth 24 h, Mars 24.66 h, Titan 15.97 days, Uranus 17.24 h). Distances are means, so the real figure varies through the year (about ±9% on Mars). Venus rotates backwards, so the Sun sets in the east there. Uranus rotates backwards on its side, so where the Sun sets changes with its seasons, and the 4.8 s holds only at equinox: about 35 s at solstice, and at high latitudes the Sun does not set for years. The Sun is drawn at true relative size between worlds, Earth = 1 (minimum 2 px, so distant Suns can be enlarged), but not to scale with the land in the picture.

      Sources. Skies: NASA Goddard SVS 13645, Geronimo Villanueva / James Tralie, Planetary Spectrum Generator. Atmospheres: NASA planetary fact sheets and NASA’s Titan facts. Mars’s colour pattern: measured from Curiosity PIA19400 (NASA/JPL-Caltech/MSSS/Texas A&M Univ.), which is linked, not reproduced here. Ground: AI-generated images. This page was not made by NASA and NASA does not endorse it; no NASA logo is used, and NASA’s video and its soundtrack are not used.

      Quick guide

      Use cases, answers, and nearby tools

      Compact below-tool notes that help first-run users and repeated visitors move faster without changing the main interface.

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      How to use

      Run a clean first pass

      1. The page opens on dusk on Mars with the Sun about to touch the horizon. Drag the picture up or down for the progress of the sunset, and the Sun follows. Drag left or right to change your distance from the Sun, from Venus out to Uranus; where a disc shows, the Sun is smaller the further out you go.
      2. Tap a frame in the film strip to change world — Earth (clear, hazy, overcast), Mars, Venus, Titan, Uranus. In all seven the Sun has gone the same way towards setting, and the readout gives the Sun’s apparent size, the atmosphere and how long the Sun takes to sink its own diameter.
      3. To see the real thing, press “See Curiosity’s real photograph” for NASA’s page. Press “Save card” to keep a 1200×630 image, labelled with what is simulated and what is AI-imagined.

      Examples

      Real jobs this page helps with

      • Why Martian sunsets are blueOpen the default page: blue-white around the Sun, fading to grey-blue. Follow the link to compare Curiosity’s real photograph; the page also says the hue here is adjusted.
      • Titan’s gold hazeTap Titan and drag through dusk: the sky is gold with no crisp Sun disc, and distant land fades into the haze.
      • The Sun from UranusOpen ?w=uranus&p=50: Uranus has no ground and the Sun is a bright point, 0.052 times its size on Earth. Press “Run every Sun on one clock”: at equinox it is down in 4.8 seconds, Earth’s takes 2.1 minutes and Venus’s 5.7 hours, and 60× or 3600× lets you watch them all finish.
      • A teacher comparing atmospheresDrag to the middle of dusk on a projector and point along the film strip: all seven skies with the Sun at the same point on the way to setting, with composition and pressure beside them, then the five Suns on one scale.
      • Save a moment as a share cardPick a world and a moment (say Venus at 20%) and press “Save card” for a 1200×630 image with its sources and URL; opening the same link shows the same moment.

      FAQ

      What people usually want to know

      Why are sunsets blue on Mars?

      According to NASA JPL’s caption of Curiosity’s photograph, fine dust in the Martian atmosphere lets blue light through more efficiently, so blue stays close to the Sun while yellow and red scatter more widely. The effect is strongest at sunset because the light path is longest. That photograph’s colour is calibrated and white-balanced, and the Mastcam camera is slightly less sensitive to blue than human eyes.

      Are these real photographs?

      No. Sky colours come from NASA Goddard’s atmospheric simulation, the ground on Mars, Venus and Titan is an AI-imagined picture generated from a text description, and the Sun, the sea and Uranus’s clouds are this page’s own drawing. No spacecraft photograph is shown here; on Mars a link takes you to NASA’s page for Curiosity’s real sunset.

      Why is the colour on Mars adjusted?

      NASA’s simulated table for Mars runs from tan to a pale tone that clips to white near the Sun, which hides the blue a rover actually recorded. So from mid-dusk on Mars this page changes the hue: the brightness is still the simulation’s, while the colour follows the pattern measured in Curiosity’s photograph, blue-white near the Sun and fading to grey-blue. It is this page’s adjustment, not NASA’s output, and the label on the picture says “regraded”.

      Is every planet hazy? How do the atmospheres differ?

      No. Mars has about 0.006 bar of 95% carbon dioxide, thin air with fine dust. Venus has 92 bar of 96.5% carbon dioxide, and sulfuric-acid cloud hides the Sun from far overhead rather than lying on the ground as fog, but air that dense scatters strongly by itself, so distant land fades there too. Titan has about 1.5 bar, about 95% nitrogen and 5% methane, with thick orange haze that blurs distant land. Uranus is 82.5% hydrogen and 15% helium with no ground.

      How big is the Sun from other worlds, and how long does a sunset take?

      The Sun’s apparent diameter falls with distance: about 0.74° from Venus (1.38× Earth’s), 0.53° from Earth, 0.35° from Mars (about two thirds), 0.056° from Titan and only 0.028° from Uranus, where it is a bright point. At the equator the Sun takes about 2.1 minutes to sink its own diameter on Earth, 1.4 minutes on Mars, 3.6 minutes on Titan and about 4.8 seconds on Uranus (rotation only, ignoring its tilted axis, so the real figure can differ a lot), but about 5.7 hours on Venus — and Venus rotates backwards, so the Sun sets in the east.

      Are the Sun’s height and the brightness accurate?

      No, both are schematic. NASA does not state where the Sun is in each frame, so dragging up and down moves through its frames, and the percentage is how far the Sun has gone towards this page’s estimate of that world’s sunset, not an elevation angle. The brightness is not true brightness either: Titan’s surface is far darker in reality and Venus’s is dimmer and more orange, as the label on the picture says. Sun sizes use each world’s mean distance from the Sun.