Quick Stats


Moon Facts

Bulk parameters
 
Moon
 
Ratio
(Moon/Earth)
Mass (1024 kg) 0.07349 0.0123
Volume (1010 km3)2.1958 0.0203
Equatorial radius (km)1738.1 0.2725
Polar radius (km)1736.00.2731
Volumetric mean radius (km)1737.1 0.2727
Ellipticity (Flattening) 0.0012 0.36
Mean density (kg/m3) 3350 0.607
Surface gravity (m/s2) 1.62 0.165
Surface acceleration (m/s2)1.62 0.166
Escape velocity (km/s) 2.38 0.213
GM (x 106 km3/s2) 0.0049 0.0123
Bond albedo0.11 0.360
Visual geometric albedo0.12 0.330
Visual magnitude V(1,0) +0.21 -
Solar irradiance (W/m2)1367.6 1.000
Black-body temperature (K) 270.7 1.064
Topographic range (km)16 0.800
Moment of inertia (I/MR2)0.394 1.191
Orbital parameters (for orbit about the Earth)
Semimajor axis (106 km) 0.3844
Perigee (106 km)*0.3633
Apogee (106 km)* 0.4055
Revolution period (days) 27.3217
Synodic period (days) 29.53
Mean orbital velocity (km/s)1.023
Max. orbital velocity (km/s) 1.076
Min. orbital velocity (km/s) 0.964
Inclination to ecliptic (deg) 5.145
Inclination to equator (deg) 18.28 – 28.58
Orbit eccentricity 0.0549
Sidereal rotation period (hrs)655.728
Obliquity to orbit (deg)6.68
Recession rate from Earth (cm/yr)3.8
Mean values at opposition from Earth
Mean Distance from Earth’s equator (km) 378,000
Apogee (km) 357,000
Perigee407,000
Apparent diameter (seconds of arc)1896
Apparent visual magnitude -12.74
Lunar Atmosphere
Diurnal temperature range: 100 K to <400 K (roughly -250 F to +250 F)
Total mass of atmosphere:~25,000 kg
Surface pressure (night):3 × 10-15 bar (2 × 10-12 torr)
Abundance at surface:2 × 105 particles/cm3


Estimated Composition in particles per cubic cm:
Helium 4 (4He) – 40,000 ; Neon 20 (20Ne) – 40,000 ; Hydrogen (H2) – 35,000
Argon 40 (40Ar) – 30,000 ; Neon 22 (22Ne) – 5,000 ; Argon 36 (36Ar) – 2,000
Methane – 1000 ; Ammonia – 1000 ; Carbon Dioxide (CO2) – 1000
Trace Oxygen (O+), Aluminum (Al+), Silicon (Si+)
Possible Phosphorus (P+), Sodium (Na+), Magnesium (Mg+)


Composition of the tenuous lunar atmosphere is poorly known and variable, these are estimates of the upper limits of the nighttime ambient atmosphere composition. Daytime levels were difficult to measure due to heating and outgassing of Apollo surface experiments.

Tags:
moon planetary satellite

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