Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.

Site Tools

  • AAAS
  • Subscribe
  • Feedback

Site Search

Search Advanced

Science 29 November 1974:
Vol. 186. no. 4166, pp. 825 - 826
DOI: 10.1126/science.186.4166.825

Articles

Lunar Magnetic Field: Permanent and Induced Dipole Moments

C. T. Russell 1, P. J. Coleman Jr. 1, and G. Schubert 1

1 Space Science Center, University of California, Los Angeles 90024

Apollo 15 subsatellite magnetic field observations have been used to measure both the permanent and the induced lunar dipole moments. Although only an upper limit of 1.3 x 1018 gauss-cubic centimeters has been determined for the permanent dipole moment in the orbital plane, there is a significant induced dipole moment which opposes the applied field, indicating the existence of a weak lunar ionosphere.


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
The Moon: Sources of the Crustal Magnetic Anomalies.
L. L. Hood, L. L. HOOD, P. J. COLEMAN JR., and D. E. WILHELMS (1979)
Science 204, 53-57
   Abstract »    PDF »
The Ancient Lunar Core Dynamo.
S. K. Runcorn and S. K. RUNCORN (1978)
Science 199, 771-773
   Abstract »    PDF »



ADVERTISEMENT
Click Me!

ADVERTISEMENT
Click Me!

To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)