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| 1 | Statistical research on the motion properties of the magnetotail current sheet:Cluster observations显示文摘The origin of the flapping motion of the earth's magnetotail current sheet is one of the most important problems in the magnetotail dynamics.Using Cluster data,we make a statistical research on the motion properties of the magnetotail current sheet of 2001 and 2003.We calculate the velocities of the magnetotail current sheet using new methods and obtain the distribution of the magnetotail current sheet velocities in the X-Y plane in GSE coordinate system.Our results show that although most of the current sheets were propagating toward the tail flanks and those of the exceptions lay in dusk side,which is consistent with previous studies,the proportions of the current sheet which were propagating toward midnight (where |YGSE|=0) were higher than those in previous studies.Motions of the current sheet in the middle area (|YGSE|<8 Re) of the magnetotail are investigated.Relatively high value of the Z component of the velocity further confirms that the middle area of the magnetotail might be a source region for the motion of the current sheets which were propagating towards the tail flanks.According to our case studies,the way the current sheets propagated toward midnight area differs significantly from that toward dusk and dawn side,from which we infer that there might be two different kinds of current sheet motions originated from different sources.The statistical results of this paper may give some clues for further studies on the origin of the flapping motion of the magnetotail current sheet. | H.REME E.LUCEK | 2010 | Science China(Technological Sciences)2010，53，6： | 5 |
| 2 | THEMIS observations of two substorms on February 26,2008显示文摘Two substorms occurred at ~04:05 and ~04:55 UT on February 26,2008 are studied with the in-situ observations of THEMIS satellites and ground-based aurora and magnetic field measurements.Angelopoulos et al.have made a comprehensive study of the 04:55 UT event.We showed detailed features of the two substorms with much attention to the first event and to the rela-tionship between mid-tail magnetic reconnection(MR) and substorm activities.It was found that in the earlier stage of each substorm,a first auroral intensification occurred 2-3 min soon after the start of mid-tail MR,followed by a slow and very lim-ited expansion.The auroral arcs were weak,short-lived,and localized,characterizing all features of a pseudobreakup.We re-garded the first auroral brightening as the initial onset of the substorms.A few minutes later,a second stronger auroral intensification appeared,followed by quick and extensive expansions.It was interesting to note that the second brightening and related poleward expansion happened almost simultaneously(within a couple of minutes) with the onset of earthward flow and dipolarization in the near-Earth tail and other phenomenon of the substorm expansion phase.We thus regarded the second auroral brightening as the major onset of the substorms.Furthermore,it was seen that during the growth phase of the two substorms,the polar cap open flux Ψ kept increasing,while it quickly reduced during the substorm expansion and recovery phase.These variations of Ψ implied that the evolution of the two substorm expansion phases were closely related to MR of tail lobe open field lines.Analysis of substorm activities revealed that the two events studied were small substorms;while estimate of MR rate indicated that the MR processes in the two substorms were weak.The aforementioned observations suggested that mid-tail MR initiated the pseudobreakup first;the earthward flow generated by MR transported magnetic flux and energy to the near-Earth tail to cause the formation of SCW and CD,which induced near-Earth dipolarization and major auroral brightening,and eventually led to the onset of the substorm expansion phase.These results were clearly consistent with the picture of NENL and RCS models and supported the two step initiation scenario of substorms. | CHU XiangNing PU ZuYin CAO Xin WANG Jue V.MISHIN V.ANGELOPOULOS LIU Jiang WEI Yong K.H.GLASSMEIER J.MCFADDEN D.LARSON S.MENDE H.FREY C.T.RUSSELL I.MANN D.SIBECK ZONG QiuGang FU SuiYan XIE Lun T.I.SAIFUDINOVA M.V.TOLOCHKO L.A.SAPRONOVA H.REME E.LUCEK | 2010 | Science China(Technological Sciences)2010，53，5： | 3 |
| 3 | 极尖区电离层离子与地磁活动及太阳风的相关分析显示文摘对2001~2003年间Cluster星簇穿越极尖区期间观测到的电离层起源的离子(O+离子,He+离子和H+离子)特性进行了统计分析,主要研究了这些离子的数密度与地磁活动以及太阳风动压之间的关系.结果表明:O+离子数密度和地磁活动指数Kp之间存在着正相关关系,He+离子数密度和地磁活动指数Kp不相关,O+离子和He+离子数密度都和太阳风动压之间存在着显著的正相关关系;H+离子数密度与太阳风动压之间存在着正相关关系,而和地磁活动指数Kp不相关.最后,对这些离子的特性与太阳风动压及地磁活动之间的关系进行了讨论. | 郭建广 史建魁 T.L.Zhang 刘振兴 A.Fazakerley H.Rème I.Dandouras E.Lucek | 2007 | 科学通报2007，52，3： | 2 |
| 4 | 行星际磁场与磁尾磁通量绳形成的关系显示文摘收集了Cluster卫星在2001-2005年间观测到的磁尾磁通量绳事件,并对磁通量绳(magnetic flux rope)形成及其内部磁场结构与行星际磁场(IMF)的关系作了统计研究.考虑磁通量绳被观测到时行星际磁场的条件,在所有73个磁通量绳事件中,行星际磁场By分量占有主导地位的事件有80%,且78%的事件具有与行星际磁场By分量相同方向的核心场.行星际磁场通过在磁层顶与地球磁场相互作用改变南北等离子体片内磁场相对方向,形成有利于磁通量绳形成的磁场位形,并且行星际磁场By分量的方向对磁通量绳内部核心场的方向具有决定性影响.从统计结果来看,磁通量绳的形成并不会依赖于行星际磁场Bz分量的方向. | 张永存 刘振兴 沈超 E.Lucek H.Réme | 2008 | 空间科学学报2008，28，2： | 2 |
| 5 | 太阳风在地球激波前兆区减速的统计研究显示文摘本文首次利用完全相同两颗卫星(CLUSTER C1和C3)的数据对地球激波前兆区太阳风的减速和偏转特性进行了统计研究.结果表明,在激波前兆坐标系中,太阳风减小的速度随观测点到激波的距离D_(BS)增大而减小,随行星际磁场与激波法向夹角θ_(BN)增大也减小,在ULF波动区深度D_(WS)小于6R_e(R_e为地球半径)的范围内最为显著;伴随着太阳风减速的另外一个现象——太阳风的偏转,也存在相似的规律.其最大减速和最大偏转角度分别为10 km/s和3°.太阳风减速和偏转,以及随之变化的太阳风动压,可能会引起地球磁层顶位置和形状发生改变,同时也为激波前兆区弥散(diffuse)离子的起源及加热提供了一种可能的机制. | 符慧山 曹晋滨 张铁龙 H.Reme E.Lucek | 2009 | 地球物理学报2009，52，4： | 1 |
| 6 | Cluster卫星对磁尾电流片运动特性的统计分析显示文摘地球磁尾电流片拍动的起源和运动方式一直是磁尾动力学研究中的重要问题之一.本文利用Cluster卫星数据,统计分析了2001年和2003年的磁尾电流片运动特性,利用我们最近发展的分析结构特征方向和运动速度的新方法,计算了磁尾电流片的运动速度,并给出了磁尾电流片在GSE坐标系中XY平面内的速度分布图.我们发现磁尾电流片存在着两种不同性质的运动,除了磁尾电流片向晨昏方向的运动,分析表明,磁尾电流片还存在着明显朝向子夜方向的运动(即GSE坐标系中Y=0平面).观测还进一步表明,位于磁尾中间区域(|Y_GSE|<8Re)的电流片的扰动,其南北向的速度分量相对较大,这从另一个方面说明磁尾中性片的中间区域可能是导致大部分磁尾电流片拍动事件中电流片朝向晨昏两侧运动的源区.对于运动方向朝向子夜方向(Y=0平面)的电流片,其运动方式与运动方向朝向晨昏两侧的电流片存在着明显的不同,因此我们推测,它们应具有不同的起源.本文的统计结果,为我们深入研究地球磁尾电流片拍动源区等物理问题提供了的参考依据. | 孙为杰 史全岐 傅绥燕 宗秋刚 濮祖荫 谢伦 肖婷 李蕾 刘振兴 H.Reme E.Lucek | 2010 | 中国科学:技术科学2010，40，7： | 1 |
| 7 | THEMIS星座对2008年2月26日磁层亚暴的观测--磁尾重联触发的亚暴分析研究显示文摘本文利用THEMIS卫星结合地面极光和地磁的观测,研究了2008年2月26日04:05和04:55UT的两次亚暴事件.Angelopoulos已经对发生在04:55UT的第二个亚暴事件做了分析.本文对两次亚暴的相关活动进行了详细研究,特别对第一次做了深入讨论,并着重分析了磁重联与亚暴活动的关系.在两次亚暴的初始阶段,第一次极光增亮发生在中磁尾磁重联后2~3min,但是持续时间较短,极向膨胀缓慢,与伪暴的特征相似,标志了亚暴的初突发(initial onset).两次亚暴都存在第二次极光增亮和极光的极向膨胀,且时间与近地磁尾观测的地向流和磁场偶极化同时发生,并与亚暴膨胀相的其他活动的发生同步,标志了亚暴的主突发(major onset).在两次亚暴的增长相期间,极盖区开放磁通量持续增加;在亚暴膨胀相和恢复相中,极盖区磁通量迅速减少.表明两次亚暴膨胀相的演化分别与两次尾瓣开放磁力线重联过程相联系的.从亚暴活动的参数分析,这两次亚暴都属于小亚暴范围;从重联率分析,两次磁重联都属于弱重联.本文的观测结果表明,中磁尾磁尾重联首先触发伪暴;高速流将磁通量和能量传输到近地磁尾;高速流减速最终导致亚暴电流楔(substorm current wedge,简称SCW)的形成和电流中断,产生近地偶极化和极光膨胀,引起亚暴膨胀相突发.本文的观测结果是对近地中性线模型(near earth neutral line,简称NENL)和重联-电流中断协同模型(synthesis scenario of MR and CD,简称RCS)模型及亚暴膨胀相两步突发观点的有力支持. | 褚项宁 濮祖荫 曹馨 V.MISHIN 王珏 魏勇 宗秋刚 傅绥燕 谢伦 V.ANGELOPOULOS 刘江 K.H.GLASSMEIER J.MCFADDEN D.LARSON S.MENDE H.FREY C.T.RUSSELL I.MANN D.SIBECK T.I.SAIFUDINOVA M.V.TOLOCHKO L.A.SAPRONOVA H.REME E.LUCEK | 2010 | 中国科学:技术科学2010，40，5： | 0 |
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