The solar wind is the driving force of space weather on Earth. Energy can be stored in the Earth's magnetosphere and will subsequently be released. These so called substorms are not only cause for the spectacle we know as the aurora, but have also the potential to cause serious harm to modern technology. Particularly in view of the reliance of today's society on digital communication delivered by satellites has made this a major concern in the last few decades.Heating and expansion of the atmosphere by the aurora can lead to an increase in drag on satellites, possibly reducing lifespan, warranting course correction or at the very least cause observations of the changed course to avoid collisions (Marcos et al., 2010). Geomagnetically induced currents can affect man-made electrically conducting structures such as the power-grid, under-sea communication cables or pipelines, causing disruption in various services (Pirjola, 2000). GNSS systems can provide exact timing and location services, based on the distance to the satellite calculated from the known position and travel time of the signal to a ground based receiver. However, ionospheric disturbances can change the travel time by several nanoseconds or few microseconds, giving errors in the position by a few meters (Kintner et al., 2007).Although there is the potential for global events to occur, these are extremely rare and localized events are much more likely. In order to mitigate the risks, it is important to know when and where they will occur.Originally based on images (Akasofu, 1964;Akasofu et al., 1965), the study of substorms has moved on to satellite-supported studies (McPherron et al., 1973), giving us the currently used model of substorms. The solar wind has long since been identified as the main driving force behind substorms (Caan et al., 1975). A rapid northward turning of the Interplanetary Magnetic Field (IMF) B z component was believed to be the main trigger behind substorms, however this has been disproven in recent years (Freeman & Morley, 2009;Johnson & Wing, 2014;P. T. Newell & Liou, 2011). During the growth phase of substorms, energy is stored in the Earth's magnetosphere. This energy is released during the expansion phase and the magnetosphere subsequently returns to its steady state in the recovery phase of a substorm.Different phases during a substorm can trigger different mechanism of energy-release which will in turn have different outcomes on the visible aurora (