Fractal analysis of Michelson Doppler Imager magnetograms: A contribution to the study of the formation of solar active regions

Authors
Citation
N. Meunier, Fractal analysis of Michelson Doppler Imager magnetograms: A contribution to the study of the formation of solar active regions, ASTROPHYS J, 515(2), 1999, pp. 801-811
Citations number
18
Categorie Soggetti
Space Sciences
Journal title
ASTROPHYSICAL JOURNAL
ISSN journal
0004637X → ACNP
Volume
515
Issue
2
Year of publication
1999
Part
1
Pages
801 - 811
Database
ISI
SICI code
0004-637X(19990420)515:2<801:FAOMDI>2.0.ZU;2-S
Abstract
In this paper a fractal analysis of active regions observed by the Michelso n Doppler Imager (MDI) instrument on the SOHO spacecraft is performed. The purpose of such an analysis is to study the shape of these magnetic regions via their fractal dimension, which characterizes their complexity, and to deduce some information on the processes that led to their formation. Both full disk and high-resolution MDI magnetograms are used and the fractal dim ensions using the perimeter/area relation (d(1)) and the linear size/area r elation (d(2)) are calculated. A statistical analysis of the estimate of a fractal dimension is performed, as well as that of the influence of noise o n it. The fractal dimension for a range of sizes is calculated. The fractal dimension d(1) is found to increase with the area of the active regions (f rom 1.48 for supergranular size structures to 1.68 for the largest structur es). The fractal dimension d(2) also increases with the area of the active regions (from 1.78 to 1.94). The fractal dimension d(1) decreases with the magnetic threshold for moderate sizes and increases for the largest structu res. The high-resolution results match those of full disk magnetograms when the images are degraded. This fractal analysis is performed in relation to the size distribution properties: the two analyses provide complementary i nformation. Then some models of active regions very similar to those of Wen tzel & Seiden are introduced to interpret the observations in terms of a pe rcolation process at the bottom of the convective zone and diffusion at the surface. These models lead to structures that are more complex than the ob served structures.