Other
Scientific paper
Aug 2009
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009jgra..11408102l&link_type=abstract
Journal of Geophysical Research, Volume 114, Issue A8, CiteID A08102
Other
2
Geochemistry: Composition Of The Moon (7811), Geochemistry: Composition Of The Moon (2723, 7526), Geochemistry: Composition Of The Moon (2109), Geochemistry: Composition Of The Moon
Scientific paper
In the present paper, we first examine some interplanetary directional discontinuities with very small B n /B (<0.1) using intraspacecraft timing method. It is found that the velocity and magnetic field fluctuations of these directional discontinuities satisfy the Walén relation. We suggest that these directional discontinuities are rotational discontinuities. In addition, we investigate the stability of interplanetary rotational discontinuities using one-dimensional hybrid simulations and found that rotational discontinuities with all values of B n /B can stably exist in the solar wind. In one simulation run, we find that the rotational discontinuity (RD) is still stable when the ratio, B n /B, equals 0.0001. Finally, from one-dimensional hybrid simulation, we further find that the ratio is significantly reduced after interaction with interplanetary fast shocks. There are a few mechanisms for generation of RDs. Among them, two mechanisms are well accepted. One is nonlinear evolution of Alfvén waves in the solar wind, and another is magnetic reconnection near the solar surface. For magnetic reconnection, the reconnection rate, V 1n/V A1(= B n /B), in the magnetosphere and solar wind, is usually <0.2. Therefore the generated RDs also have B n /B < 0.2. On the other hand, the nonlinear evolution of Alfvén waves in the solar wind can generate RDs at all values of B n /B, which contradicts to the Cluster results. We suggest that interplanetary RDs with small B n /B are likely been generated through magnetic reconnection.
Chao Jerry K.
Chen Jacqueline H.
Lee Clarence L.
Lin Chaney
Tsai Chih-Ling
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