Interface region imaging spectrograph (IRIS) observations of the fractal dimension in the solar atmosphere

We focus here on impulsive phenomena and Quiet-Sun features in the solar transition region, observed with the Interface Region Imaging Spectrograph (IRIS) at 1,400 Å (at formation temperatures of Te ≈ 104–106 K). Summarizing additional literature values we find the following fractal dimensions (in i...

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Main Authors: Markus J. Aschwanden, Nived Vilangot Nhalil
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-11-01
Series:Frontiers in Astronomy and Space Sciences
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fspas.2022.999319/full
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author Markus J. Aschwanden
Nived Vilangot Nhalil
author_facet Markus J. Aschwanden
Nived Vilangot Nhalil
author_sort Markus J. Aschwanden
collection DOAJ
description We focus here on impulsive phenomena and Quiet-Sun features in the solar transition region, observed with the Interface Region Imaging Spectrograph (IRIS) at 1,400 Å (at formation temperatures of Te ≈ 104–106 K). Summarizing additional literature values we find the following fractal dimensions (in increasing order): DA = 1.23 ± 0.09 for photospheric granulation, DA =1.40 ± 0.09 for chromospheric (network) patterns, DA = 1.54 ± 0.04 for plages in the transition region, DA = 1.56 ± 0.08 for extreme ultra-violet (EUV) nanoflares, DA = 1.59 ± 0.20 for active regions in photospheric magnetograms, and DA = 1.76 ± 0.14 for large solar flares. We interpret low values of the fractal dimension (1.0 ≲ DA ≲ 1.5) in terms of sparse curvi-linear flow patterns, while high values of the fractal dimension (1.5 ≲ DA ≲ 2.0) indicate quasi-space-filling transport processes, such as chromospheric evaporation in flares. Phenomena in the solar transition region appear to be consistent with self-organized criticality (SOC) models, based on their fractality and their size distributions of fractal areas A and (radiative) energies E, which show power law slopes of αAobs=2.51±0.21 (with αAtheo=2.33 predicted), and αEobs=2.03±0.18 (with αEtheo=1.80 predicted). This agreement suggests that brightenings detected with IRIS at 1,400 Å reveal the same nonlinear SOC statistics as their coronal counterparts in EUV.
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spelling doaj.art-3d4545b4ed9442c683a0e2b4b495ff702022-12-22T03:57:28ZengFrontiers Media S.A.Frontiers in Astronomy and Space Sciences2296-987X2022-11-01910.3389/fspas.2022.999319999319Interface region imaging spectrograph (IRIS) observations of the fractal dimension in the solar atmosphereMarkus J. Aschwanden0Nived Vilangot Nhalil1Lockheed Martin, Solar and Astrophysics Laboratory (LMSAL), Advanced Technology Center (ATC), Palo Alto, CA, United StatesArmagh Observatory and Planetarium, College Hill, Armagh, United KingdomWe focus here on impulsive phenomena and Quiet-Sun features in the solar transition region, observed with the Interface Region Imaging Spectrograph (IRIS) at 1,400 Å (at formation temperatures of Te ≈ 104–106 K). Summarizing additional literature values we find the following fractal dimensions (in increasing order): DA = 1.23 ± 0.09 for photospheric granulation, DA =1.40 ± 0.09 for chromospheric (network) patterns, DA = 1.54 ± 0.04 for plages in the transition region, DA = 1.56 ± 0.08 for extreme ultra-violet (EUV) nanoflares, DA = 1.59 ± 0.20 for active regions in photospheric magnetograms, and DA = 1.76 ± 0.14 for large solar flares. We interpret low values of the fractal dimension (1.0 ≲ DA ≲ 1.5) in terms of sparse curvi-linear flow patterns, while high values of the fractal dimension (1.5 ≲ DA ≲ 2.0) indicate quasi-space-filling transport processes, such as chromospheric evaporation in flares. Phenomena in the solar transition region appear to be consistent with self-organized criticality (SOC) models, based on their fractality and their size distributions of fractal areas A and (radiative) energies E, which show power law slopes of αAobs=2.51±0.21 (with αAtheo=2.33 predicted), and αEobs=2.03±0.18 (with αEtheo=1.80 predicted). This agreement suggests that brightenings detected with IRIS at 1,400 Å reveal the same nonlinear SOC statistics as their coronal counterparts in EUV.https://www.frontiersin.org/articles/10.3389/fspas.2022.999319/fullmethodsstatistical -fractal dimension -suntransition region -solar granulation -solar photospherefractal dimensionstatistical
spellingShingle Markus J. Aschwanden
Nived Vilangot Nhalil
Interface region imaging spectrograph (IRIS) observations of the fractal dimension in the solar atmosphere
Frontiers in Astronomy and Space Sciences
methods
statistical -fractal dimension -sun
transition region -solar granulation -solar photosphere
fractal dimension
statistical
title Interface region imaging spectrograph (IRIS) observations of the fractal dimension in the solar atmosphere
title_full Interface region imaging spectrograph (IRIS) observations of the fractal dimension in the solar atmosphere
title_fullStr Interface region imaging spectrograph (IRIS) observations of the fractal dimension in the solar atmosphere
title_full_unstemmed Interface region imaging spectrograph (IRIS) observations of the fractal dimension in the solar atmosphere
title_short Interface region imaging spectrograph (IRIS) observations of the fractal dimension in the solar atmosphere
title_sort interface region imaging spectrograph iris observations of the fractal dimension in the solar atmosphere
topic methods
statistical -fractal dimension -sun
transition region -solar granulation -solar photosphere
fractal dimension
statistical
url https://www.frontiersin.org/articles/10.3389/fspas.2022.999319/full
work_keys_str_mv AT markusjaschwanden interfaceregionimagingspectrographirisobservationsofthefractaldimensioninthesolaratmosphere
AT nivedvilangotnhalil interfaceregionimagingspectrographirisobservationsofthefractaldimensioninthesolaratmosphere