Magnetic Reconnections in a Low and a High Solar Activity Year

When there is a temporary disturbance of earth’s magnetosphere, then a geomagnetic storm (or solar storm) has occurred. It is caused by a solar wind shock wave and/or cloud of a magnetic field that interacts with the Earth's magnetic fields. The interaction of Interplanetary Magnetic Fields (IMF) of the sun with the earth’s magnetic fields in opposite directions is known as magnetic reconnection (Yousif, 2014). Magnetic reconnection (often referred as "reconnection") is the breaking and reconnecting of oppositely directed magnetic field lines in plasma at a neutral point which leads to converting the magnetic field energy into plasma kinetic and thermal energy. It occurs either in the day-time (day reconnection) where the sunward convection near the polar cusps allows energised particles to be transmitted earthward or night-time (tail reconnection) where particles injected into the magnetosphere are saturated, thus releasing stored energy in the form of auroral substorms. Sokolov (2011) suggested that a geomagnetic storm can be determined by changes in the Disturbed-storm time (Dst). However, not all geomagnetic storms have an initial phase and not all sudden increase in Dst or SYM-H are followed by a geomagnetic storm. This paper attempts to determine what are responsible for magnetic reconnections in the solar cycle 24 considering a low solar activity year 2009 and a high solar activity year 2012. We have to classify the geomagnetic storms using the Dst indices and rearrange the IMF Bz according to its negative, neutral and positive values. We measured the correlation between Bz and solar wind using a 1-min resolution OMNIweb dataset. Thereafter, establish the factors responsible for magnetic reconnections. We analysed 39 and 202 geomagnetic storms in 2009 and 2012 respectively considering the Dst indices and IMF Bz values of each month obtained from the OMNIWeb Database. Our results showed that geomagnetic storms occurred in 10% and 45% of days in the year 2009 and 2012 respectively which implies they were frequent and intense due to high solar activity caused by the frequent occurrence of coronal mass ejections (CMEs) and interplanetary coronal mass ejections (ICMEs) in the year 2012 than in the year 2009. This study also revealed that negative Bz occurrences were 47.54% and 52.18% in 2009 and 2012 respectively. Thus, the more intense the geomagnetic storms, the more Bz would go south and the more magnetic reconnections and subsequently auroral substorms which can increase radiation doses for occupants of transpolar flights, disruption of shortwave radio communications, distortion of compass readings in polar regions, failure of electrical transmission lines, increased corrosion in long pipelines, anomalies in the operations of communications satellites, and potentially lethal dosages of radiation for astronauts in interplanetary spacecraft.