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国家自然科学基金(10425312)

作品数:3 被引量:1H指数:1
相关作者:吴德金王德焴冯恒强孙令鹏更多>>
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Suprathermal particle events observed by WIND spacecraft in interplanetary space during 1995―1999 and their classification被引量:1
2008年
Fifty-five suprathermal particle events were selected from WIND observations between 1995 and 1999. Based on systematic analysis on the observational characteristics of these events a two-parameter (the rising time and the flux ratio of electrons to protons in each event) classification method was proposed to classify these events. The three clas-sified classes are (1) impulsive electron events with the flux ratio of electrons to protons being bigger than 1 and rising time being shorter than 200 min, (2) impulsive proton events with the flux ratio being smaller than 1 and rising time being shorter than 200 min, and (3) gradual proton events with the flux ratio being smaller than 1 and the rising time being longer than 200 min. In the past, "impulsive solar electron events" were under in-tense research. However, because the selection standards of their velocity dispersions or pitch-angle distributions were inadequate, statistical surveys of selected events were dif-ferent from each other and even some conclusions were not consistent with the theory, for example, the relation of type-III solar radio bursts to the "impulsive solar electron events". The first class of impulsive electron events are associated with type-III radio bursts and with clear velocity dispersions; therefore they ought to originate from the Sun. The second class of the events, which have short continuance time and usually are not associated with type-III radio bursts and without velocity dispersion, are still far away from inter-planetary shocks and most of them do not one-to-one correspond to corrotating interact-ing regions (CIRs); such events are possible results of local interplanetary magnetic field reconnection or electromagnetic disturbances. Finally, about 2/3 gradual proton events of the third class occur with interplanetary shocks, the delay times of which are almost equal to the rising time. Some of these events can be understood as particle accelerations by shocks.
SUN LingPeng1,2, WU DeJin1 & WANG DeYu1 1 Purple Mountain Observatory, Chinese Academy of Sciences, Nanjing 210008, China
关键词:SOLARWINDSOLARERUPTIVEINTERPLANETARYREGIONS
通过建立自然坐标系确定磁云边界方法的探讨
2006年
通常卫星探测到的关于行星际空间磁场的数据都是在GSE坐标系(地心太阳黄道坐标系)里表示出来的.磁云是行星际日冕物质抛射事件的一个重要子集,它们的边界认证一直是磁云研究中感兴趣的问题之一.通过讨论坐标系转换确定磁云边界的方法,由磁云的磁通量管特征建立磁云自然坐标系,然后把行星际空间的磁场转换到磁云自然坐标系里.在磁云自然坐标系里磁云作为一个磁通量管的结构能够清晰地显示出来.结合磁云的等离子体特征就可以比较容易地把磁云和背景太阳风分辨出来,即确定了磁云的边界.
冯恒强吴德金赵寄昆
关键词:太阳
WIND卫星1995到1999年间在行星际空间观测的超热粒子事件及其分类
2009年
根据WIND卫星在1995~1999年间的行星际观测资料,检索了55个行星际超热粒子事件.在对这些事件观测特征进行系统分析的基础上进一步提出了行星际超热粒子事件的双参量(上升时间和电子-离子流量比)分类方法.选取适当的阀值,这些事件可划分为三类:1)脉冲型超热电子事件(上升时间小于200min,电子质子比流量大于1);2)脉冲型超热质子事件(上升时间小于200min,电子质子比流量小于1);3)缓变型超热质子事件(上升时间大于200min,电子质子比流量小于1).第一类事件全部都具有速度弥散并伴随太阳Ⅲ型暴,应该都是太阳起源的;第二类事件总的持续时间都很短,而且都远离行星际激波,多数也不与共转相互作用区对应,这类事件不伴随Ⅲ型暴,没有速度弥散,可能仅仅是当地行星际磁重联,或电磁场扰动的结果;第三类事件约2/3尾随着行星际激波,激波的延迟时间约等于它们的上升时间,用激波加速可以解释部分现象.
孙令鹏吴德金王德焴
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