Ann. Geophys., 30, 379–387, 2012 www.ann-geophys.net/30/379/2012/ Annales doi:10.5194/angeo-30-379-2012 Geophysicae © Author(s) 2012. CC Attribution 3.0 License. Global magnetospheric response to an interplanetary shock: THEMIS observations H. Zhang1, D. G. Sibeck2, Q.-G. Zong3,4, J. P. McFadden5, D. Larson5, K.-H. Glassmeier6, and V. Angelopoulos7 1Geophysical Institute, University of Alaska Fairbanks, AK, USA 2NASA Goddard Space Flight Center, Greenbelt, MD, USA 3Center for Atmospheric Research, University of Massachusetts, Lowell, USA 4Institute of Space Physics and Applied Technology, Peking University, Beijing, China 5Space Sciences Laboratory, University of California, Berkeley, CA, USA 6Institute for Geopysics and Extraterrestrial Physics, TU Braunschweig, Germany 7IGPP/ESS UCLA, Los Angeles, CA 90095-1567, USA Correspondence to: H. Zhang (
[email protected]) Received: 21 July 2011 – Revised: 3 January 2012 – Accepted: 8 February 2012 – Published: 22 February 2012 Abstract. We investigate the global response of the geospace 1 Introduction plasma environment to an interplanetary (IP) shock at ∼02:24 UT on 28 May 2008 from multiple THEMIS space- The interaction of interplanetary (IP) shocks (usually fast craft observations in the magnetosheath (THEMIS B and forward shocks) with the magnetosphere includes several C), the mid-afternoon magnetosphere (THEMIS A), and the phases, including interaction with the bow shock, transmis- dusk magnetosphere (THEMIS D and E). The interaction of sion through the magnetosheath, interaction with the mag- the transmitted IP shock with the magnetosphere has global netopause, transmission into the magnetosphere as fast and effects. Consequently, it can affect geospace plasma signif- intermediate mode waves, modifications of the field-aligned icantly.