Titan's highly dynamic magnetic environment: A systematic survey of Cassini magnetometer observations from flybys TA-T62

被引:62
作者
Simon, Sven [1 ]
Wennmacher, Alexandre [1 ]
Neubauer, Fritz M. [1 ]
Bertucci, Cesar L. [2 ,3 ]
Kriegel, Hendrik [4 ]
Saur, Joachim [1 ]
Russell, Christopher T. [5 ]
Dougherty, Michele K. [3 ]
机构
[1] Univ Cologne, Inst Geophys & Meteorol, D-5000 Cologne 41, Germany
[2] Univ Buenos Aires, CONICET, Inst Astron & Space Phys, Buenos Aires, DF, Argentina
[3] Univ London Imperial Coll Sci Technol & Med, Blackett Lab, Space & Atmospher Phys Grp, London SW7 2AZ, England
[4] TU Braunschweig, Inst Theoret Phys, Braunschweig, Germany
[5] Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90024 USA
关键词
Titan; Saturn's magnetosphere; Magnetodisk current sheet and lobes; Cassini flybys; Plasma interaction with unmagnetized bodies; HYBRID SIMULATION; MAGNETOSPHERE; PLASMA; ATMOSPHERE; ENCELADUS;
D O I
10.1016/j.pss.2010.04.021
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We analyze the variability of the ambient magnetic field near Titan during Cassini encounters TA-T62 (October 2004-October 2009). Cassini magnetometer (MAG) data show that the moon's magnetic environment is strongly affected by its proximity to Saturn's warped and highly dynamic magnetodisk. In the nightside sector of Saturn's magnetosphere, the magnetic field near Titan is controlled by intense vertical flapping motions of the magnetodisk current sheet, alternately exposing the moon to radially stretched lobe-type fields and to more dipolar, but highly distorted current sheet fields. In southern summer, when most of the Cassini encounters took place, the magnetodisk current sheet was on average located above Titan's orbital plane. However, around equinox in August 2009, the distortions of Titan's magnetic environment due to the rapidly moving current sheet reached a maximum, thus suggesting that the equilibrium position of the sheet at that time was significantly closer to the moon's orbital plane. In the dayside magnetosphere, the formation of the magnetodisk lobes is partially suppressed due to the proximity of the magnetopause. Therefore, during most encounters that took place near noon, Titan was embedded in highly distorted current sheet fields. Within the framework of this study, we not only provide a systematic classification of all Titan flybys between October 2004 and October 2009 as lobe-type or current sheet scenarios, but we also calculate the magnetospheric background field near Titan's orbit whenever possible. Our results show that so far, there is not a single Cassini flyby that matches the frequently applied picture of Titan's plasma interaction from the pre-Cassini era (background field homogeneous, stationary and perpendicular to the moon's orbital plane). The time scales upon which the ambient magnetospheric field close to Titan undergoes significant changes range between only a few minutes and up to several hours. The implications for the development of numerical models for Titan's local plasma interaction are discussed as well. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1230 / 1251
页数:22
相关论文
共 33 条
  • [1] Mass of Saturn's magnetodisc:: Cassini observations
    Arridge, C. S.
    Russell, C. T.
    Khurana, K. K.
    Achilleos, N.
    Andre, N.
    Rymer, A. M.
    Dougherty, M. K.
    Coates, A. J.
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2007, 34 (09)
  • [2] Thermal electron periodicities at 20RS in Saturn's magnetosphere
    Arridge, C. S.
    Andre, N.
    Achilleos, N.
    Khurana, K. K.
    Bertucci, C. L.
    Gilbert, L. K.
    Lewis, G. R.
    Coates, A. J.
    Dougherty, M. K.
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2008, 35 (15)
  • [3] Saturn's magnetodisc current sheet
    Arridge, C. S.
    Russell, C. T.
    Khurana, K. K.
    Achilleos, N.
    Cowley, S. W. H.
    Dougherty, M. K.
    Southwood, D. J.
    Bunce, E. J.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2008, 113 (A4)
  • [4] Warping of Saturn's magnetospheric and magnetotail current sheets
    Arridge, C. S.
    Khurana, K. K.
    Russell, C. T.
    Southwood, D. J.
    Achilleos, N.
    Dougherty, M. K.
    Coates, A. J.
    Leinweber, H. K.
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2008, 113 (A8)
  • [5] Titan's magnetic field signature during the first Cassini encounter
    Backes, H
    Neubauer, FM
    Dougherty, MK
    Achilleos, N
    André, N
    Arridge, CS
    Bertucci, C
    Jones, GH
    Khurana, KK
    Russell, CT
    Wennmacher, A
    [J]. SCIENCE, 2005, 308 (5724) : 992 - 995
  • [6] BACKES H, 2005, THESIS U KOLN
  • [7] The magnetic memory of Titan's ionized atmosphere
    Bertucci, C.
    Achilleos, N.
    Dougherty, M. K.
    Modolo, R.
    Coates, A. J.
    Szego, K.
    Masters, A.
    Ma, Y.
    Neubauer, F. M.
    Garnier, P.
    Wahlund, J. -E.
    Young, D. T.
    [J]. SCIENCE, 2008, 321 (5895) : 1475 - 1478
  • [8] The variability of Titan's magnetic environment
    Bertucci, C.
    Sinclair, B.
    Achilleos, N.
    Hunt, P.
    Dougherty, M. K.
    Arridge, C. S.
    [J]. PLANETARY AND SPACE SCIENCE, 2009, 57 (14-15) : 1813 - 1820
  • [9] Characteristics and variability of Titan's magnetic environment
    Bertucci, Cesar L.
    [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 2009, 367 (1889): : 789 - 798
  • [10] Identification of a dynamic atmosphere at Enceladus with the Cassini magnetometer
    Dougherty, MK
    Khurana, KK
    Neubauer, FM
    Russell, CT
    Saur, J
    Leisner, JS
    Burton, ME
    [J]. SCIENCE, 2006, 311 (5766) : 1406 - 1409