Abstract

Separating active regions that are quiet from potentially eruptive ones is a key issue in Space Weather applications. Traditional classification schemes such as Mount Wilson and McIntosh have been effective in relating an active region large scale magnetic configuration to its ability to produce eruptive events. However, their qualitative nature prevents systematic studies of an active region's evolution for example. We introduce a new clustering of active regions that is based on the local geometry observed in Line of Sight magnetogram and continuum images. We use a reduced-dimension representation of an active region that is obtained by factoring the corresponding data matrix comprised of local image patches. Two factorizations can be compared via the definition of appropriate metrics on the resulting factors. The distances obtained from these metrics are then used to cluster the active regions. We find that these metrics result in natural clusterings of active regions. The clusterings are related to large scale descriptors of an active region such as its size, its local magnetic field distribution, and its complexity as measured by the Mount Wilson classification scheme. We also find that including data focused on the neutral line of an active region can result in an increased correspondence between our clustering results and other active region descriptors such as the Mount Wilson classifications and the $R$ value. We provide some recommendations for which metrics, matrix factorization techniques, and regions of interest to use to study active regions.

Highlights

  • Identifying properties of active regions (ARs) that are necessary and sufficient for the production of energetic events such as solar flares is one of the key issues in space weather

  • We find that including data focused on the neutral line of an active region can result in an increased correspondence between our clustering results and other active region descriptors such as the Mount Wilson classifications and the R-value

  • We introduce a reduced-dimension representation of an AR that allows a data-driven unsupervised classification of ARs based on their local geometry

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Summary

Introduction

Identifying properties of active regions (ARs) that are necessary and sufficient for the production of energetic events such as solar flares is one of the key issues in space weather. The Mount Wilson classification (see Table 1 for a brief description of its four main classes) has been effective in relating a sunspot’s large scale magnetic configuration with its ability to produce flares. Several studies showed that a large proportion of all major flare events begin with a d configuration (Warwick 1966; Mayfield & Lawrence 1985; Sammis et al 2000). The Mount Wilson classification is generally carried out manually which results in human bias. Several papers (Colak & Qahwaji 2008, 2009; Stenning et al 2013) have used supervised techniques to reproduce the Mount Wilson and other schemes which has resulted in a reduction in human bias

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