The magnetic memory of Titan's ionized atmosphere

After 3 years and 31 close flybys of Titan by the Cassini Orbiter, Titan was finally observed in the shocked solar wind, outside of Saturn's magnetosphere. These observations revealed that Titan's flow-induced magnetosphere was populated by "fossil" fields originating from Saturn...

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Autor principal: Bertucci, César Luis Fermín
Otros Autores: 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
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 2008
Acceso en línea:Registro en Scopus
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Registro en la Biblioteca Digital
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100 1 |a Bertucci, César Luis Fermín 
245 1 4 |a The magnetic memory of Titan's ionized atmosphere 
260 |c 2008 
270 1 0 |m Bertucci, C.; Instituto de Astronomica Y Fisica del Espacio, Ciudad Universitaria, Buenos Aires, Argentina; email: cbertucci@iafe.uba.ar 
504 |a Neubauer, F.M., Gurnett, D.A., Scudder, J.D., Hartle, R.E., (1984) Saturn, pp. 760-787. , T. Gehrels, M. S. Matthews, Eds, Univ. of Arizona Press, Tucson, AZ 
504 |a Wahlund, J.-E., (2005) Science, 308, p. 986 
504 |a Ness, N.F., Acuña, M.H., Behannon, K.W., (1982) J. Geophys. Res, 87, p. 1369 
504 |a Backes, H., (2005) Science, 308, p. 992 
504 |a Szego, K., (2007) Geophys. Res. Lett, 34, pp. L24S03 
504 |a Kivelson, M.G., (2006) Science, 311, p. 1391 
504 |a SLT is measured from the noon meridian in the direction of Saturn's rotation; PSW = ρv2, where ρ and v, , are the solar wind density and speed, respectively 
504 |a All times are expressed in UT; Dougherty, M.K., (2004) Space Sci. Rev, 114, p. 331 
504 |a In the Saturn-centered spherical solar magnetic coordinate system (KSMAG, the polar axis coincides with planet's magnetic axis and λKSMAG and φKSMAG are, respectively, the magnetic field latitude and azimuth φKSMAG, 0 corresponds to the magnetic noon meridian; RMP = PSW -1/4.3, where RMP is the magnetopause's standoff distance; Arridge, C.S., (2006) J. Geophys. Res, 111, pp. A11227 
504 |a Masters, A., (2008) J. Geophys. Res, , 10.1029/2008JA013276 
504 |a Gurnett, D.A., (2004) Space Sci. Rev, 114, p. 395 
504 |a Young, D.T., (2004) Space Sci. Rev, 114, p. 1 
504 |a In the Titan-centered spherical ionospheric interaction coordinate system (TIIS, the equatorial plane contains the direction to Saturn (Y TIIS) and that of the nominal corotation flow (X TIIS, λTIIS and φTIIS are, respectively, the latitude and azimuth measured from XTIIS toward YTIIS; McAndrews, H.J., (2008) J. Geophys. Res, 113, pp. A04210 
504 |a Hartle, R.E., (2006) Geophys. Res. Lett, 33, pp. L08201 
504 |a H. Backes, thesis, University of Cologne, Germany (2005); Niedner, M.B., Brandt, J.C., (1978) Astrophys. J, 223, p. 655 
504 |a Coates, A.J., (2007) Geophys. Res. Lett, 34, pp. L24S05 
504 |a We thank A. Balogh, T. Horbury, W. S. Kurth, C. Mazelle, S. J. Schwartz, and C. T. Russell for useful discussions, and N. Powell for artwork. C.B. was supported by a Science and Technology Facilities Council Postdoctoral Fellowship 
506 |2 openaire  |e Política editorial 
520 3 |a After 3 years and 31 close flybys of Titan by the Cassini Orbiter, Titan was finally observed in the shocked solar wind, outside of Saturn's magnetosphere. These observations revealed that Titan's flow-induced magnetosphere was populated by "fossil" fields originating from Saturn, to which the satellite was exposed before its excursion through the magnetopause. In addition, strong magnetic shear observed at the edge of Titan's induced magnetosphere suggests that reconnection may have been involved in the replacement of the fossil fields by the interplanetary magnetic field.  |l eng 
593 |a Space and Atmospheric Physics Group, Imperial College London, Blackett Laboratory, Prince Consort Road, London SW7 2AZ, United Kingdom 
593 |a Atmospheric Physics Laboratory, Department of Physics and Astronomy, University College London, Gower Street, London WC1E 6BT, United Kingdom 
593 |a Centre for Planetary Sciences, University College London, United Kingdom 
593 |a Department of Physics and Astronomy, University of Iowa, 613 Van Allen Hall, Iowa City, IA 52242-1479, United States 
593 |a Mullard Space Science Laboratory, University College London, Holmbury St. Mary, Dorking, Surrey RH5 6NT, United Kingdom 
593 |a KFKI Research Institute for Particle and Nuclear Physics, Building III, Konkoly Thege Street 29-33, H-1121 Budapest, Hungary 
593 |a Institute of Geophysics and Planetary Physics, University of California Los Angeles, Los Angeles, CA 90025, United States 
593 |a Institute for Geophysics and Meterology, Köln University, 50923 Köln, Germany 
593 |a Swedish Institute of Space Physics, Box 537, SE-751 21 Uppsala, Sweden 
593 |a Southwest Research Institute, Post Office Box 28510, San Antonio, TX 78227-1301, United States 
593 |a Instituto de Astronomica Y Fisica del Espacio, Ciudad Universitaria, Buenos Aires, Argentina 
690 1 0 |a MAGNETIC FIELD 
690 1 0 |a MAGNETOPAUSE 
690 1 0 |a MAGNETOSPHERE 
690 1 0 |a PLANETARY ATMOSPHERE 
690 1 0 |a SATURN 
690 1 0 |a SOLAR WIND 
690 1 0 |a TITAN 
690 1 0 |a ARTICLE 
690 1 0 |a ATMOSPHERE 
690 1 0 |a GEOMETRY 
690 1 0 |a MAGNETIC FIELD 
690 1 0 |a MAGNETISM 
690 1 0 |a PRIORITY JOURNAL 
700 1 |a Achilleos, N. 
700 1 |a Dougherty, M.K. 
700 1 |a Modolo, R. 
700 1 |a Coates, A.J. 
700 1 |a Szego, K. 
700 1 |a Masters, A. 
700 1 |a Ma, Y. 
700 1 |a Neubauer, F.M. 
700 1 |a Garnier, P. 
700 1 |a Wahlund, J.-E. 
700 1 |a Young, D.T. 
773 0 |d 2008  |g v. 321  |h pp. 1475-1478  |k n. 5895  |p Science  |x 00368075  |w (AR-BaUEN)CENRE-344  |t Science 
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