TABLE OF THE PLANETS AND SUN



Planet


D(AU)1
Rotation2

Period

Orbital

Period

Axis3

Tilt

Radius4

(x RE)

Mass5

(x ME)

MD6

(x MD, E)

Dipole7

Tilt

Number*

of Moons

Sun 0.000 25 days# N/A 7.25o& 109+ 332,000 X$ X$ N/A
Mercury 0.387 58.7 days 88 days ~0o 0.382 0.055 ~4.7x10-4 ~10o 0
Venus 0.723 243 days 225 days -2o 0.949 0.815 N/A N/A 0
Earth 1.000 23.9 hrs 365 days 23.5o 1.000 1.000 1.000 11.5o 1
Mars 1.520 24.6 hrs 1.88 yrs 24o 0.533 0.107 ? ? 2
Jupiter 5.200 9.92 hrs 11.9 yrs 3.1o 11.200 318 20,000 9.6o 28
Saturn 9.540 10.7 hrs 29.5 yrs 29o 9.450 95.200 540 0.7o 18
Uranus 19.200 -17.29hrs 84.0 yrs -82.1o 4.100 14.600 48 59o 17
Neptune 30.100 16.11 hrs 165 yrs 28.8o 3.880 17.200 26 47o 8
Pluto 39.400 6.39 days 248 yrs >50o? ~0.24 0.002 N.K.* N.K.* 1

Footnotes:

1 D(AU) is the planet's average distance from the Sun in units of A.U. See the glossary.

2 Rotation period is given in a "fixed" (i.e., non rotating) coordinate system with respect to the stars.

3 Tilt of the planet's rotation axis compared to a line perpendicular to its orbital plane.

4 The Earth's average radius at its equator, RE = 6378 km (or 3963 miles).

5 The Earth's mass ME = 5, 977, 000, 000, 000, 000, 000, 000, 000 kg.

6 The planet's magnetic dipole moment, which is a measure of the main part of its magnetic field, its dipole field, in units of MD,E, the Earth's Dipole moment, which is 79, 000, 000, 000, 000, 000, 000, 000, 000 Gauss-cm^3.

7 The dipole tilt is the angle between the planet's magnetic dipole axis and its rotation axis.

8 Number of known moons per planet; the total is 64 moons.

* N.K. means "not known."

# Rotation at the Sun's equator. It is slower at higher latitudes.

& Tilt of the rotation axis with respect to the Ecliptic plane.

+ The radius of the Sun refers to the radius of its photosphere.

$ The Sun's magnetic dipole moment and dipole tilt angle are highly variable. In fact, the dipole moment changes polarity approximately every 11 years. It is usually not too useful to describe only the dipole of the Sun when describing the Sun's magnetism, whose field geometry is very complicated.


This table is a modified, extended, and updated version of a table on the characteristics of the planets published by the Astronomical Society of the Pacific (1983).

Green Line
Site created: April 25, 1997 Last Modified: December 12, 2003

Curator: Albert E. Davison, International Technology and Management, Inc.
E-mail: Albert.E.Davison@gsfc.nasa.gov

Responsible NASA Representative: Dr. Michael Collier
E-mail: Michael.R.Collier@nasa.gov