Statistical investigation of the Auroral oval boundaries using IMAGE WIC
Master thesis
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https://hdl.handle.net/11250/3153574Utgivelsesdato
2024-06-03Metadata
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- Master theses [179]
Sammendrag
The aurora is a visible effect of Earth’s coupling to the Sun, it appears in an approximate oval form over the magnetic poles. The aurora moves to lower latitudes as thegeomagnetic activity increases, and the poleward boundary of the aurora marks theopen-closed field line boundary (OCB). The location of the OCB is important as it canhelp determine reconnection rates and predict global-scale space weather. In this thesisI use a dataset created by Ohma et al. (2024a) to investigate how variations in theauroral oval equatorial (EB) and poleward (PB) boundaries are described for differentsolar wind and magnetic indices. In addition, I conduct a superposed epoch analysis toinvestigate the boundaries movement during substorms. I focus on the magnetic indicesP, open flux content of the polar cap, dP/dt, the rate of change in open flux, A, theclosed magnetic flux in the auroral oval, and dA/dt the rate of change in closed flux. Inaddition Milan et al. (2012)’s solar wind-magnetosphere coupling function ΦD was usedas a proxy for dayside reconnection. I find a surprisingly low correlation between P,dP/dt, and ΦD for small values of the nightside reconnection proxy AL and its rate ofchange dAL/dt. I show that for the region between 0230 and 0500 MLT, the average PBdoes not move equatorward as Kp increases. I demonstrate how the so-called HeppnerMaynard-Boundary (HMB) and EB are well correlated with a maximum correlationvalue of 0.67. I find an increased bulge at the onset location during winter, and surprisingly I find the PC to be thinner for all MLTs except between 2100-2300 during thesummer. We find that the PB is moderately correlated with ΦD, the EB could be usedto find the HMB, and A and P are well explained on average by ΦD during substorms.Characterizing large-scale variations in the auroral oval is crucial for comprehendingglobal geospace dynamics. These findings not only enhance our understanding but alsoillustrate the potential of future missions with auroral imaging capabilities to further advance this field.