Articles | Volume 36, issue 6
https://doi.org/10.5194/angeo-36-1537-2018
https://doi.org/10.5194/angeo-36-1537-2018
ANGEO Communicates
 | 
15 Nov 2018
ANGEO Communicates |  | 15 Nov 2018

Can an interplanetary magnetic field reach the surface of Venus?

Yasuhito Narita and Uwe Motschmann

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Cited articles

Bagdonat, T. B.: Hybrid simulations of weak comets, PhD thesis, Tech. Univ. Braunschweig, Braunschweig, 2002. a, b
Benkhoff, J., van Casteren, J., Hayakawa, H., Fujimoto, M., Laakso, H., Novara, M., Ferri, P., Middleton, H. R., and Ziethe, R.: BepiColombo – Comprehensive exploration of Mercury: Mission overview and science goals, Planet. Space Sci., 58, 2–20, https://doi.org/10.1016/j.pss.2009.09.020, 2010. a
Bößwetter, A.: Wechselwirkung des Mars mit dem Sonnenwind: Hybrid-Simulationen mit besonderem Bezug zur Wasserbilanz, PhD thesis, Tech. Univ. Braunschweig, Braunschweig, Germany, https://publikationsserver.tu-braunschweig.de/receive/dbbs_mods_00028707 (last access: 15 November 2018), 2009. a
Bößwetter, A., Bagdonat, T., Motschmann, U., and Sauer, K.: Plasma boundaries at Mars: a 3-D simulation study, Ann. Geophys., 22, 4363–4379, https://doi.org/10.5194/angeo-22-4363-2004, 2004. a, b
Dimmock, A. P., Alho, M., Kalio, E., Pope, S. A., Zhang, T. L., Kilpua, E., Pulkkinen, T. I., Futaana, Y., and Coates, A. J.: The response of the Venusian plasma environment to the passage of an iCME: Hybrid simulation results and Venus Express observations, J. Geophys. Res.-Space, 123, 3580–3601, https://doi.org/10.1029/2017JA024852, 2018. a
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Short summary
Venus has no intrinsic magnetic field. On the other hand, we discover that an interplanetary magnetic field may nevertheless penetrate the planetary ionosphere by the diffusion process and reach the planetary surface when the solar wind condition remains for a sufficiently long time, between 12 and 54 h, depending on the condition of ionosphere.