Skip Navigation

Radiation Protection Dosimetry 2005 116(1-4):50-54; doi:10.1093/rpd/nci074
This Article
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Add to My Personal Archive
Right arrow Download to citation manager
Right arrow Search for citing articles in:
ISI Web of Science (2)
Right arrowRequest Permissions
Google Scholar
Right arrow Articles by Jun, I.
Right arrow Articles by Garrett, H. B.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Jun, I.
Right arrow Articles by Garrett, H. B.
Social Bookmarking
 Add to CiteULike   Add to Connotea   Add to Del.icio.us  
What's this?

Published by Oxford University Press 2005.

Comparison of high-energy trapped particle environments at the earth and jupiter

Insoo Jun* and Henry B. Garrett

Jet Propulsion Laboratory, California Institute of Technology, Mail Stop 122-107, 4800 Oak Grove Drive, Pasadena, CA 91109, USA

* Corresponding author: insoo.jun{at}jpl.nasa.gov

The ‘Van Allen belts’ of the trapped energetic particles in the Earth's magnetosphere were discovered by the Explorer I satellite in 1958. In addition, in 1959, it was observed that UHF radio emissions from Jupiter probably had a similar source—the Jovian radiation belts. In this paper, the global characteristics of these two planets' trapped radiation environments and respective magnetospheres are compared and state-of-the-art models used to generate estimates of the high-energy electron (≥100 keV) and proton (≥1 MeV) populations—the dominant radiation particles in these environments. The models used are the AP8/AE8 series for the Earth and the Divine–Garrett/GIRE model for Jupiter. To illustrate the relative magnitude of radiation effects at each planet, radiation transport calculations were performed to compute the total ionising dose levels at the geosynchronous orbit for the Earth and at Europa (Jupiter's 4th largest moon) for Jupiter. The results show that the dose rates are ~0.1 krad(Si) d–1 at the geosynchronous orbit and ~30 krad(Si) d–1 at Europa for a 2.5 mm spherical shell aluminium shield—a factor of ~300 between the two planets.


Add to CiteULike CiteULike   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us    What's this?




Disclaimer: Please note that abstracts for content published before 1996 were created through digital scanning and may therefore not exactly replicate the text of the original print issues. All efforts have been made to ensure accuracy, but the Publisher will not be held responsible for any remaining inaccuracies. If you require any further clarification, please contact our Customer Services Department.