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GEOPHYSICS, ASTRONOMY, AND ASTROPHYSICS

ULF Waves Associated with Solar Wind Deceleration in the Earth's Foreshock

Fu Hui-Shan et al 2009 Chinese Phys. Lett. 26 119402 (4pp)   doi: 10.1088/0256-307X/26/11/119402  Help

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Fu Hui-Shan1,2, Cao Jin-Bin1,3, Yang Biao4, E Lucek5, H Rème6 and I Dandouras6
1 State Key Laboratory of Space Weather, Center for Space Science and Applied Research, Beijing 100190
2 Graduate University of Chinese Academy of Sciences, Beijing 100049
3 Beijing University of Aeronautics and Astronautics, Beijing 100190
4 Institute of Space Physics and Applied Technology, Peking University, Beijing 100871
5 Blackett Laboratory, Imperial College, Prince Consort Road, London, SW7 2BZ, UK
6 Centre d'Etude Spatiale des Rayonnements, 31028, Toulouse, France
E-mail: hsfu@spaceweather.ac.cn (Fu Hui-Shan)

Abstract. Characteristics of ULF waves associated with the solar wind deceleration in the Earth's foreshock on 6–7 April 2003 is studied using the wave telescope technique. In the satellite frame, the ULF waves are the left-handed polarized and quasi anti-parallel propagating mode, with a power peak at about 18.63 mHz. The wave vector in the GSE coordinates is estimated to be κ = (−4.29, 2.28, 1.21) × 10−4 km−1. In the solar wind frame, the frequency of waves becomes −9.39 mHz after the Doppler shift correction. The propagation direction of the waves is thus reversed and correspondingly the polarization of the waves becomes right-handed. The above-mentioned characteristics of the ULF waves in the solar wind frame indicate that the ULF waves associated with the solar wind deceleration are the Alfven-whistler waves, which have been frequently reported in both the observations and computer simulations.

PACS numbers: 94.05.Pt, 94.30.Cq, 94.30.Va

Print publication: Issue 11 (November 2009)
Received 20 July 2009

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