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Depression in cosmic ray intensity influenced by interplanetary disturbances

机译:受宇宙射线强度的抑郁受到行列间干扰的影响

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Interplanetary manifestations of coronal mass ejections with specific plasma and field properties, called "in interplanetary magnetic clouds,'' have been observed in the heliosphere since the mid terplanetary mid-1960s. Depending on their a as- ssociated features, a set of observed magnetic clouds identified at 1 AU were grouped in four different classes using sociated data over four decades: (1) interplanetary magnetic clouds moving with the ambient solar wind (MC structure), (2) magnetic clouds moving faster than the ambient solar wind and forming a shock/sheath structure of compressed plasma and field ahead of it (SMC structure), (3) magnetic c clouds "pushed'' by the high louds high-speed streams from behind, forming an interaction region between the two (MIH structure), and (4) shock shock-associated magnetic clouds followed by high high-speed streams (SMH structure). A detailed analysis has been carried out in the p present work to study the o resent on- nset times of cosmic set cosmic-ray decreases occurring during 2005 2005-06 with respect to the arrival times of interplanetary shocks and magnetic clouds. The interplanetary magnetic field strength (B), north south component of interplanetary ma mag- gne netic field (Bz), solar wind velocity (V), sunspot number (R) and disturbance storm time index (Dst) associated with ic these events have been studied in the present work. The data (neutron monitor count rate) of different cosmic ray ne neu- utron monitors have be tron been used. It is noted that on the onset of magnetic cloud the cosmic ray intensity, Bz component en of IMF, Disturbance storm time index Dst found to decrease for one day and then all the three components increases gradually, whereas interplanetary magnetic fi field B increases for one day and then decrease sharply. However the s eld so- olar wind velocity found to remain constant and sunspot number (R) increases after one day of the onset of cloud with lar some depression. This southward turning of Bz produces large geomagnet geomagnetic disturbances, which reflects in Dst value. ic Increase in Dst index, sunspot number (R) and Bz after the magnetic cloud event seems to be associated with cosmic ray intensity increase.
机译:日冕物质抛射与特定的血浆和字段属性,在星际磁云被称为”星际表现‘’已在日光中期以来terplanetary 60年代中期观察。根据他们的一个原样ssociated功能,一组观测到的磁在1 AU识别云在使用sociated数据的四个不同类别的过去四十年来被分组:(1)星际磁云与周围太阳风(MC结构),移动(2)磁云移动比周围太阳风更快,形成压缩等离子体和在它前面场(SMC结构),(3)磁ç云“由高LOUDS高速从后面流推‘’,形成两个(MI​​H结构)之间的相互作用区域的冲击/鞘结构,和随后在高高速流(SMH结构)(4)激震相关磁云。的详细分析已在p目前的工作已进行了研究宇宙组宇宙射线的邻重新发送导通NSET倍相对于星际冲击和磁云的到达时间在2005 2005-06减小发生。星际磁场强度(B),星际毫安的南北分量MAG-GNE带IC这些事件具有相关联的字段NETIC(BZ),太阳风速度(V),太阳黑子数(R)和干扰风暴时间索引(DST)研究了在目前的工作。不同宇宙射线NE neu- utron监视器的数据(中子监测器计数率)已经被TRON被使用。值得注意的是,在磁性云开始时的宇宙射线强度,BZ部件EN IMF的,扰动风暴时间索引Dst的发现减少1天,然后将所有三种组分逐渐增大,而对于一个星际磁场Fi字段乙增加一天,然后急剧下降。但是S场所谓OLAR风速发现云的发作有一天拉尔一些凹陷后保持恒定和太阳黑子数(R)的增加。这Bz的向南转向生产大geomagnet地磁扰动,这反映了DST的价值。 IC增加Dst的索引,太阳黑子数(R)和BZ磁云事件之后似乎与宇宙射线强度增加有关。

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