27-day variations of the galactic cosmic ray intensity and anisotropy in the minimum of the 23rd solar activity cycle

被引:11
|
作者
Gil, A. [1 ]
Modzelewska, R. [1 ]
Alania, M. V. [1 ,2 ]
机构
[1] Agr & Pedagog Univ Siedlce, Inst Math & Phys, PL-08110 Siedlce, Poland
[2] Georgian Acad Sci, Inst Geophys, Tbilisi, Georgia
关键词
27-day variation of the GCR intensity; 27-day variation of the GCR anisotropy; Polarity epochs of solar magnetic cycle;
D O I
10.1016/j.asr.2011.06.026
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
We study the 27-day variations of the solar wind velocity, galactic cosmic ray (GCR) intensity and anisotropy in the last minimum epoch of solar activity (2007-2009, A < 0). The average amplitude of the 27-day variation of the galactic cosmic ray anisotropy (A27A) in the current minimum epoch of solar activity (2007-2009, A < 0) is lesser than in previous positive polarity period as it is expected from the drift theory. So, polarity dependence rule for the 27-day variation of the GCR anisotropy is fully kept. It is a universal principle for the amplitudes of the 27-day variation of the GCR anisotropy. At the same time, the average amplitude of the 27-day variation of the GCR intensity (A27I) remains at the same level as for previous minimum epoch 1995-1997 (A > 0) showing by the same token an violation of its polarity dependence rule established earlier. We assume that this phenomenon could be generally related with the well established 27-day variation of the solar wind velocity being in anti-correlation with the similar changes of the 27-day variation of the GCR intensity. Generally, a character of the heliolongitudinal asymmetry of spatial large-scale structure of the solar wind velocity (SWV) established in the recent minimum epoch, preferentially pronounces in the behavior of the 27-day variation of the GCR intensity than anisotropy. The formation of the 27-day variation of the GCR anisotropy preferentially takes place in a restricted disk like local vicinity in the helioequatorial region, whilst the 27-day variation of the GCR intensity is formed in the global three dimensional vicinity of the heliosphere. (c) 2011 COSPAR. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:712 / 715
页数:4
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