Role of Impact Angle on Equatorial Electrojet (EEJ) Response to Interplanetary (IP) Shocks

被引:0
|
作者
Nilam, B. [1 ]
Ram, S. Tulasi [1 ]
Oliveira, Denny M. [2 ,3 ]
Dimri, A. P. [1 ]
机构
[1] Indian Inst Geomagnetism, Mumbai, Maharashtra, India
[2] Univ Maryland, Goddard Planetary Heliophys Inst, Baltimore, MD USA
[3] NASA, Goddard Space Flight Ctr, Geospace Phys Lab, Greenbelt, MD USA
关键词
interplanetary (IP) shocks; shock impact angle; equatorial electrojet; geomagnetic field; solar wind; GEOMAGNETICALLY INDUCED CURRENTS; PATRICKS DAY STORM; ELECTRICAL-CONDUCTIVITY; CURRENT SYSTEM; FIELDS; TIME; MAGNETOSPHERE; CONVECTION;
D O I
10.1029/2024JA032638
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Interplanetary (IP) shocks are one of the dominant solar wind structures that can significantly impact the Geospace when impinge on the Earth's magnetosphere. IP shocks severely distort the magnetosphere and induce dramatic changes in the magnetospheric currents, often leading to large disturbances in the geomagnetic field. Sudden enhancements in the solar wind dynamic pressure (PDyn) during IP shocks cause enhanced high-latitude convection electric fields which penetrate promptly to equatorial latitudes. In response, the equatorial electrojet (EEJ) current exhibits sharp changes of magnitudes primarily controlled by the change in PDyn and the local time. In this paper, we further investigated the influence of shock impact angle on the EEJ response to a large number (306) of IP shocks that occurred during 2001-2021. The results consistently show that the EEJ exhibits a heightened response to the shocks that head-on impact the magnetosphere (frontal shocks) than those with inclined impact (inclined shocks). The greater EEJ response during the frontal shocks could be due to a more intensified high-latitude convection electric field resulting from the symmetric compression of the magnetosphere. Finally, an existing empirical relation involving PDyn and local time is improved by including the effects of impact angle, which can quantitatively better predict the EEJ response to IP shocks. Solar Wind, a continuous stream of high-energy particles emanating from the Sun, is ubiquitous in interplanetary (IP) space. In unison, the energetic and/or transient eruptions on the Sun often release bursts of fast solar wind. When this fast solar wind interacts with the ambient solar wind in the IP space, a shock front is formed known as IP shock. These IP shocks (if Earth-directed) can impinge on the Earth's magnetosphere and transfer tremendous amounts of energy and momentum. As a result, the Earth's magnetic field is often severely disturbed. Severe geomagnetic disturbances are known to cause a myriad of space weather effects from the loss of satellites in space to damage of electrical power grids and transmission lines on ground. Historically, geomagnetic field disturbances are known to be more cataclysmic at high latitudes and lessen at latitudes below the auroral region. However, these disturbances again dramatically enhance at equatorial latitudes due to a unique ionospheric current system, known as equatorial electrojet (EEJ). This study provides new insights into the significant role of angle of shock impacting the magnetosphere and the resultant disturbances in EEJ. This study also derives an empirical relation to accurately estimate the EEJ disturbances during IP shocks. The angle of interplanetary (IP) shock impact on the magnetosphere plays a significant role in controlling the equatorial electrojet (EEJ) response The magnitude of EEJ change due to the impact of frontal IP shocks is significantly larger than that for the inclined shocks An improved empirical relation including the effects of impact angle is derived which provide better estimates of EEJ responses to IP shocks
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页数:10
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