Global Distribution of Crustal Magnetization Discovered by the Mars Global Surveyor MAG/ER Experiment

Author:

Acuña M. H.1,Connerney J. E. P.1,F. N.,Ness 2,Lin R. P.3,Mitchell D.3,Carlson C. W.3,McFadden J.3,Anderson K. A.3,Rème H.4,Mazelle C.4,Vignes D.4,Wasilewski P.1,Cloutier P.5

Affiliation:

1. NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA.

2. Bartol Research Institute, University of Delaware, Newark, DE 19716, USA.

3. Space Sciences Laboratory, University of California, Berkeley, CA 94720, USA.

4. Centre d'Etude Spatiale des Rayonnements, 31028 Toulouse Cedex 4, France.

5. Department of Space Physics and Astronomy, Rice University, Houston, TX, 77005, USA.

Abstract

Vector magnetic field observations of the martian crust were acquired by the Mars Global Surveyor (MGS) magnetic field experiment/electron reflectometer (MAG/ER) during the aerobraking and science phasing orbits, at altitudes between ∼100 and 200 kilometers. Magnetic field sources of multiple scales, strength, and geometry were observed. There is a correlation between the location of the sources and the ancient cratered terrain of the martian highlands. The absence of crustal magnetism near large impact basins such as Hellas and Argyre implies cessation of internal dynamo action during the early Naochian epoch (∼4 billion years ago). Sources with equivalent magnetic moments as large as 1.3 × 10 17 ampere-meter 2 in the Terra Sirenum region contribute to the development of an asymmetrical, time-variable obstacle to solar wind flow around Mars.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference21 articles.

1. M. H. Acuña et. al. Science 279 1676 (1998).

2. M. H. Acuña et. al. J. Geophys. Res. 97 7799 (1992).

3. The Mars Global Surveyor magnetic field experiment provides fast (up to 32 samples per second) and precise (12-bit) vector measurements of the ambient field over the range of 4 to 65 536 nT per axis. It includes two fluxgate magnetometers mounted at the outer edge of the articulated solar panels and an electron reflectometer mounted on the spacecraft body that measures the local electron distribution function in the range of ∼1 to 20 KeV to remotely sense the strength of magnetic fields of planetary origin at the top of the martian atmosphere. The observations reported here were acquired by the twin fluxgate magnetometer system.

4. The measurement error is determined primarily by incomplete knowledge of spacecraft-generated magnetic fields. These are associated with the electrical power system and uncompensated permanent magnets present in amplifiers mounted behind the spacecraft high gain antenna. During the cruise phase spacecraft maneuvers in a fixed solar panel orientation were used to determine the instrument offsets to an estimated accuracy of 0.5 nT. In the aerobraking orbits frequent spacecraft reconfigurations and articulations of the solar panels degrade the accuracy of the error estimate yielding the value quoted in the paper. The twin magnetometer configuration is used to identify spacecraft-generated magnetic fields and distinguish them from ambient field changes.

5. Le Mouël J. L., Courtillot V., Ducruix J., Geophys. J. R. Astron. Soc. 42, 251 (1975);

Cited by 904 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3