Solar System Worlds · Constellation Saturn System (Ecliptic)

Titan (Saturn VI)

Orbital parameters (15.945 d around Saturn), visual magnitude 8.4, 1.45-bar N2/CH4 atmosphere, hydrocarbon lakes, and observing guide for Titan.

Right Ascension (J2000.0)23h 30m 18.00s
Declination (J2000.0)-05° 00′ 00.0″
Primary ClassificationPlanetary-scale icy moon with dense nitrogen-methane atmosphere and surface lakes
Best Observing SeasonWhenever Saturn is well placed near opposition

Provenance-Backed Scientific Measurements

Every measurement below preserves its unit, uncertainty interval, observational method, reference epoch, quality status, and primary catalog source. See Uncertainty & Provenance for how competing measurements are handled.

Astrometric, Photometric, and Physical Parameters for Titan (Saturn VI)
ParameterValueUncertaintyMethod & EpochQuality StatusSource Archive
Opposition visual magnitude (V)8.4 mag8.2 to 9 magJPL planetary satellite ephemeris photometrydefinitiveNASA/JPL Solar System Dynamics & Planetary Fact Sheets
Orbital period around Saturn15.94542 d± 0.00001 dCassini & ground-based astrometric ephemeris (semi-major axis = 1,221,870 km / 20.27 R_Saturn)definitiveNASA/JPL Solar System Dynamics & Planetary Fact Sheets
Solid-surface radius0.4043 R⊕± 0.0002 R⊕Cassini radar altimetry & radio occultation (2,574.7 km — larger than Mercury!)definitiveNASA/JPL Solar System Dynamics & Planetary Fact Sheets
Satellite mass0.0225 M⊕± 0.0001 M⊕Cassini flyby radio-Doppler tracking (1.3452 × 10^23 kg, 1.83 × Moon)definitiveNASA/JPL Solar System Dynamics & Planetary Fact Sheets
Surface temperature93.7 K± 0.6 KESA Huygens lander in-situ surface measurement (−179.5 °C at 1.45 bar)definitiveNASA/JPL Solar System Dynamics & Planetary Fact Sheets
Measurement Uncertainties & Competing Solutions: Before Voyager 1's 1980 radio occultation, astronomers believed Titan was the largest moon in the Solar System because its opaque orange photochemical haze layer extends ~200–300 km above its solid surface; solid-body measurements show Ganymede (radius 2,634 km) is 2.3% larger than Titan (radius 2,574.7 km).

J2000 Equatorial Sky Chart & Culmination Altitude

The chart below plots Titan (Saturn VI Nitrogen-Atmosphere Moon) at RA 23h 30m 18.00s, Dec -05° 00′ 00.0″ within Saturn System (Ecliptic), alongside peak meridian transit altitudes for 40°N and 30°S observers. Use the RA/Dec Coordinate Converter to compute exact culmination altitude for your latitude.

J2000 Equatorial Sky Position (Saturn System (Ecliptic)) +90° 0° −90° 24h 12h RA 0h Peak Meridian Altitude 45° 40°N Lat 65° 30°S Lat RA: 23h 30m 18.00s Dec: -05° 00′ 00.0″ Epoch: J2000.0 · V = 8.4 mag First-party vector diagram derived from IAU / CDS SIMBAD / Gaia DR3 astrometry.

Astrophysical Context & Structure

Titan (Saturn VI), discovered on March 25, 1655, by Dutch astronomer Christiaan Huygens—the first planetary moon discovered after Galileo's four moons of Jupiter—is the largest satellite of Saturn and the second-largest moon in the Solar System. With a solid-surface diameter of 5,149.4 kilometers (0.404 Earth radii), Titan is physically larger than the planet Mercury (4,879 km), though its half-rock, half-water-ice interior gives it a bulk density of 1.88 g/cm³.

Titan is unique among all moons in the Solar System in possessing a dense, planet-like atmosphere: first detected spectroscopically by Gerard Kuiper in 1944 via methane absorption bands, its envelope is composed of ~94.2% molecular nitrogen (N2) and ~5.65% methane (CH4) with a surface pressure of 1.45 bars—45% higher than Earth's sea-level atmospheric pressure! Solar ultraviolet photolysis converts methane in the upper atmosphere into an orange tholin haze and ethane/acetylene clouds.

On January 14, 2005, ESA's Huygens probe parachuted through Titan's orange haze to make the first landing in the outer Solar System, photographing rounded water-ice cobbles in a dry river channel at 93.7 K (−179.5 °C). Subsequent Cassini synthetic-aperture radar maps revealed that Titan hosts a full cryogenic hydrological cycle based on liquid methane and ethane, complete with rainstorms, equatorial organic sand dunes, a global subsurface liquid-water ocean, and northern polar seas (Kraken Mare, Ligeia Mare, and Punga Mare).

Practical Visual Observing Guide

Minimum Instrument50 mm telescope (or 15×70 binoculars) to spot magnitude 8.4 Titan beside Saturn
Recommended Magnification60×–150× to track orbital position; 250×+ in 200 mm+ scope to resolve 0.8″ disk
Best Evening SeasonWhenever Saturn is well placed near opposition
  • Shining at visual magnitude 8.4, Titan is by far the easiest moon of Saturn to observe—visible in steadily mounted 10×50 or 15×70 binoculars and unmistakable in any 50–60 mm telescope at 40×–80×.
  • Titan orbits Saturn every 15.95 days (almost exactly 16 days), reaching a maximum elongation of ~3.1 arcminutes (about 4.5 ring-diameters) east and west of Saturn.
  • In a 200–300 mm telescope at 250×–350× under calm seeing, Titan resolves into a tiny 0.8-arcsecond warm orange-amber planetary disk.

Catalog Cross-Identifications & Aliases

Common Aliases: Saturn VI

Cross-Catalog Identifiers for Titan (Saturn VI)
Catalog AuthorityIdentifier
WIKIDATAQ2565
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Reference Guide

Angular Size, Separation & Field of View

How angular diameter (degrees, arcminutes, arcseconds), spherical angular separation, and small-angle physical diameter relate to telescope field of view.

Reference Guide

Apparent vs Absolute Magnitude Explained

Understand the logarithmic Pogson astronomical magnitude scale, apparent visual magnitude (m), absolute magnitude (M at 10 parsecs), and bolometric corrections.

Scientific Sources & Dataset Provenance

  • NASA/JPL Solar System Dynamics & Planetary Fact Sheets (DE441 (2021/2026)): Park, R. S., et al. 2021, AJ, 161, 105 (The JPL Planetary and Lunar Ephemerides DE440 and DE441) — NASA Jet Propulsion Laboratory / GSFC