Abstract

Abstract. Recent work has shown that solar wind dynamic pressure changes can have a dramatic effect on the particle precipitation in the high-latitude ionosphere. It has also been noted that the preexisting interplanetary magnetic field (IMF) orientation can significantly affect the resulting changes in the size, location, and intensity of the auroral oval. Here we focus on the effect of pressure pulses on the size of the auroral oval. We use particle precipitation data from up to four Defense Meteorological Satellite Program (DMSP) spacecraft and simultaneous POLAR Ultra-Violet Imager (UVI) images to examine three events of solar wind pressure fronts impacting the magnetosphere under two IMF orientations, IMF strongly southward and IMF Bz nearly zero before the pressure jump. We show that the amount of change in the oval and polar cap sizes and the local time extent of the change depends strongly on IMF conditions prior to the pressure enhancement. Under steady southward IMF, a remarkable poleward widening of the oval at all magnetic local times and shrinking of the polar cap are observed after the increase in solar wind pressure. When the IMF Bz is nearly zero before the pressure pulse, a poleward widening of the oval is observed mostly on the nightside while the dayside remains unchanged. We interpret these differences in terms of enhanced magnetospheric reconnection and convection induced by the pressure change. When the IMF is southward for a long time before the pressure jump, open magnetic flux is accumulated in the tail and strong convection exists in the magnetosphere. The compression results in a great enhancement of reconnection across the tail which, coupled with an increase of magnetospheric convection, leads to a dramatic poleward expansion of the oval at all MLTs (dayside and nightside). For near-zero IMF Bz before the pulse the open flux in the tail, available for closing through reconnection, is smaller. This, in combination with the weaker magnetospheric convection, leads to a more limited poleward expansion of the oval, mostly on the nightside. Key words. Magnetospheric physics (solar windmagnetosphere interactions; magnetospheric configuration and dynamics; auroral phenomena)

Highlights

  • The solar wind and the accompanying interplanetary magnetic field (IMF) are the main drivers of the dynamics of the terrestrial magnetosphere

  • In order to better understand the behavior of the auroral oval in this near-zero preceding IMF Bz scenario and test the generality of the results obtained for the 2 October 1998 event, we examine two more events of this kind

  • We argue that most of the polar cap shrinkage is associated with increased nightside reconnection, and that the strength and magnetic local times (MLTs) extent of this enhanced magnetotail reconnection depends on the previous state of the magnetosphere

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Summary

Introduction

The solar wind and the accompanying interplanetary magnetic field (IMF) are the main drivers of the dynamics of the terrestrial magnetosphere. Zesta et al (2000) and Lyons (2000) presented POLAR UVI measurements of the Northern Hemisphere nightside polar region during the period of the above pressure pulse They showed a significant increase in auroral emissions at around 10:50 UT, accompanied by a poleward motion of the high-latitude auroral boundary (up to 10◦ at some MLTs) and a widening of the auroral oval at all visible MLTs. The UV emissions dropped to their prepulse levels at around 11:20 UT, coincident with the solar wind pressure drop. In order to better understand the behavior of the auroral oval in this near-zero preceding IMF Bz scenario and test the generality of the results obtained for the 2 October 1998 event, we examine two more events of this kind

Event 1: 6 January 1998
30 April 1998
Findings
Conclusions
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