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Detailed Moon Statistics
Moon / Earth Comparisons

Bulk Parameters
Moon
Earth
Ratio (Moon/Earth)
Mass (1024 kg)
0.07349
5.9736
0.0123
Volume (1010 km3)
2.1968
108.321
0.0203
Equatorial radius (km)
1737.4
6378.1
0.2724
Polar radius (km)
1737.4
6356.8
0.2733
Volumetric mean radius (km)
1737.4
6371.0
0.2727
Ellipticity (Flattening)
0.000
0.00335
0.0
Mean density (kg/m3)
3340
5515
0.605
Surface gravity (m/s2)
1.62
9.78
0.166
Escape velocity (km/s)
2.38
11.2
0.213
GM (x 106 km3/s2)
0.0049
0.3986
0.0123
Bond albedo
0.11
0.306
0.360

Visual geometric albedo
0.12
0.367
0.330

Visual magnitude V(1,0)
+0.21
-3.86
-
Solar irradiance (W/m2)
1367.6
1367.6
1.000
Black-body temperature (K)
274.5
254.3
1.079
Topographic range (km)
16
20
0.800
Moment of inertia (I/MR2)
0.394
0.3308
1.191
J2 (x 10-6)
202.7
1082.63
0.187

Orbital parameters for the Moon (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
Orbit inclination (deg)     5.145
Orbit eccentricity     0.0549
Sidereal rotation period (hrs)     655.728
Equatorial inclination (deg)     6.68
Recession rate from Earth (cm/yr)     3.8

Mean values at opposition from Earth
Distance from Earth (km)     384,467
Apparent diameter (seconds of arc)     1864.2
        Apparent visual magnitude     -12.74


Lunar Atmosphere

Diurnal temperature range: >100 K to <400 K  (roughly -173 C to +227 C)
Total mass of atmosphere:  ~25,000 kg
Surface pressure (night): 3 x 10-15 bar  (2 x 10-12 torr)
Abundance at surface: 2 x 105 particles/cm3

Estimated Composition (particles per cubic cm):
    4He - 40,000 ; 20Ne - 40,000 ; H2 - 35,000
    40Ar - 30,000 ; 22Ne - 5,000 ; 36Ar - 2,000
    Methane - 1000 ; Ammonia - 1000 ; CO2 - 1000
    Trace O+, Al+, Si+
    Possible P+, Na+, Mg+

Composition of the tenuous lunar atmosphere is poorly known and variable;
these are estimates of the upper limits of the night time ambient atmosphere
composition.  Daytime levels are difficult to measure due to heating and
outgassing of Apollo surface experiments (Detailed Earth Statistics)

The Moon
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