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Solar Wind Turbulence and Complexity Probed with Rank-Ordered Multifractal Analysis (ROMA)
The Rank-Ordered Multifractal Analysis (ROMA) is a tool designed to characterize scale (in)variance and multifractality based on rank ordering the fluctuations in "groups" characterized by the same mono-fractal behavior (Hurst exponent). A range-limited structure-function analysis provides...
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Published in: | Entropy (Basel, Switzerland) Switzerland), 2024-10, Vol.26 (11), p.929 |
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description | The Rank-Ordered Multifractal Analysis (ROMA) is a tool designed to characterize scale (in)variance and multifractality based on rank ordering the fluctuations in "groups" characterized by the same mono-fractal behavior (Hurst exponent). A range-limited structure-function analysis provides the mono-fractal index for each rank-ordered range of fluctuations. We discuss here two examples of multi-scale solar wind turbulence and complexity where ROMA is applied on the following: (a) data collected by Ulysses spacecraft in the fast solar wind, outside the ecliptic, between 25 and 31 January 2007, at roughly 2.5 Astronomical Units (AU) from the Sun, in the Southern heliosphere, at latitudes between -76.5 and -77.3 degrees, and (b) slow solar wind data collected in the ecliptic plane by Venus Express spacecraft, at 0.72 AU, on 28 January 2007. The ROMA spectrum of fast solar wind derived from ULYSSES data shows a scale-dependent structure of fluctuations: (1) at the smallest/kinetic range of scales (800 to 3200 km), persistent fluctuations are dominant, and (2) at the inertial range of scales (10
to 2 × 10
km), anti-persistent fluctuations are dominant, but less clearly developed and possibly indicative for the development of instabilities with cross-over behavior. The ROMA spectrum of the slow solar wind derived from Venus Express data, suggests a different structure of turbulence: (1) fully developed multifractal turbulence across scales between 5 × 10
and 4 × 10
km, with the Hurst index changing from anti-persistent to persistent values for the larger amplitude magnetic fluctuations; (2) at the smallest scales (400 to 6400 km), fluctuations are mainly anti-persistent, and the ROMA spectrum indicates a tendency towards mono-fractal behavior. |
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to 2 × 10
km), anti-persistent fluctuations are dominant, but less clearly developed and possibly indicative for the development of instabilities with cross-over behavior. The ROMA spectrum of the slow solar wind derived from Venus Express data, suggests a different structure of turbulence: (1) fully developed multifractal turbulence across scales between 5 × 10
and 4 × 10
km, with the Hurst index changing from anti-persistent to persistent values for the larger amplitude magnetic fluctuations; (2) at the smallest scales (400 to 6400 km), fluctuations are mainly anti-persistent, and the ROMA spectrum indicates a tendency towards mono-fractal behavior.</description><identifier>ISSN: 1099-4300</identifier><identifier>EISSN: 1099-4300</identifier><identifier>DOI: 10.3390/e26110929</identifier><identifier>PMID: 39593874</identifier><language>eng</language><publisher>Switzerland: MDPI AG</publisher><subject>Celestial bodies ; Charged particles ; Complexity ; Data analysis ; Ecliptic ; Energy ; Fractal analysis ; Fractals ; Function analysis ; Heliosphere ; Hypotheses ; intermittency ; Magnetic fields ; Magnetic variations ; multifractal analysis ; Plasma ; rank-ordered multifractal analysis ; River networks ; Solar wind ; Spacecraft ; Turbulence ; Venus Express (ESA)</subject><ispartof>Entropy (Basel, Switzerland), 2024-10, Vol.26 (11), p.929</ispartof><rights>2024 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>2024 by the authors. 2024</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c360t-c9bcc75d3855fc7d2b6ff22e2716c4a0c4fbb4eb034622217c67a62e08de54b13</cites><orcidid>0000-0002-9474-7468 ; 0000-0003-3604-2352 ; 0000-0001-7038-9494 ; 0000-0002-5294-0075</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/3133003874/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/3133003874?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>230,314,723,776,780,860,881,2096,25730,27900,27901,36988,36989,44565,53765,53767,75095</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/39593874$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Echim, Marius</creatorcontrib><creatorcontrib>Munteanu, Costel</creatorcontrib><creatorcontrib>Voitcu, Gabriel</creatorcontrib><creatorcontrib>Teodorescu, Eliza</creatorcontrib><title>Solar Wind Turbulence and Complexity Probed with Rank-Ordered Multifractal Analysis (ROMA)</title><title>Entropy (Basel, Switzerland)</title><addtitle>Entropy (Basel)</addtitle><description>The Rank-Ordered Multifractal Analysis (ROMA) is a tool designed to characterize scale (in)variance and multifractality based on rank ordering the fluctuations in "groups" characterized by the same mono-fractal behavior (Hurst exponent). A range-limited structure-function analysis provides the mono-fractal index for each rank-ordered range of fluctuations. We discuss here two examples of multi-scale solar wind turbulence and complexity where ROMA is applied on the following: (a) data collected by Ulysses spacecraft in the fast solar wind, outside the ecliptic, between 25 and 31 January 2007, at roughly 2.5 Astronomical Units (AU) from the Sun, in the Southern heliosphere, at latitudes between -76.5 and -77.3 degrees, and (b) slow solar wind data collected in the ecliptic plane by Venus Express spacecraft, at 0.72 AU, on 28 January 2007. The ROMA spectrum of fast solar wind derived from ULYSSES data shows a scale-dependent structure of fluctuations: (1) at the smallest/kinetic range of scales (800 to 3200 km), persistent fluctuations are dominant, and (2) at the inertial range of scales (10
to 2 × 10
km), anti-persistent fluctuations are dominant, but less clearly developed and possibly indicative for the development of instabilities with cross-over behavior. The ROMA spectrum of the slow solar wind derived from Venus Express data, suggests a different structure of turbulence: (1) fully developed multifractal turbulence across scales between 5 × 10
and 4 × 10
km, with the Hurst index changing from anti-persistent to persistent values for the larger amplitude magnetic fluctuations; (2) at the smallest scales (400 to 6400 km), fluctuations are mainly anti-persistent, and the ROMA spectrum indicates a tendency towards mono-fractal behavior.</description><subject>Celestial bodies</subject><subject>Charged particles</subject><subject>Complexity</subject><subject>Data analysis</subject><subject>Ecliptic</subject><subject>Energy</subject><subject>Fractal analysis</subject><subject>Fractals</subject><subject>Function analysis</subject><subject>Heliosphere</subject><subject>Hypotheses</subject><subject>intermittency</subject><subject>Magnetic fields</subject><subject>Magnetic variations</subject><subject>multifractal analysis</subject><subject>Plasma</subject><subject>rank-ordered multifractal analysis</subject><subject>River networks</subject><subject>Solar wind</subject><subject>Spacecraft</subject><subject>Turbulence</subject><subject>Venus Express (ESA)</subject><issn>1099-4300</issn><issn>1099-4300</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNpdkU1vEzEQhlcIREvhwB9AK3FpDwv-3viEooiPSq2CShESF8sf49bBWaf2LpB_j0tK1HIae-bRo9G8TfMSozeUSvQWiMAYSSIfNYe1yo5RhB7fex80z0pZIUQoweJpc0All3TWs8Pm-5cUdW6_hcG1l1M2U4TBQqvrd5HWmwi_w7htP-dkwLW_wnjdXujhR7fMDnLtnE9xDD5rO-rYzgcdtyWU9vhieT4_ed488ToWeHFXj5qvH95fLj51Z8uPp4v5WWepQGNnpbG2547OOPe2d8QI7wkB0mNhmUaWeWMYGESZIITg3opeCwJo5oAzg-lRc7rzuqRXapPDWuetSjqov42Ur5TOY7ARlHQIG-Z4D9ozSbjpvUYgiUNGMI5Ydb3buTaTWYOzMIxZxwfSh5MhXKur9FNhXC9KsKyG4ztDTjcTlFGtQ7EQox4gTUVRTCnDVHBa0df_oas05XrEHYXQbUSVOtlRNqdSMvj9Nhip2_jVPv7Kvrq__p78lzf9A1GyqUU</recordid><startdate>20241030</startdate><enddate>20241030</enddate><creator>Echim, Marius</creator><creator>Munteanu, Costel</creator><creator>Voitcu, Gabriel</creator><creator>Teodorescu, Eliza</creator><general>MDPI AG</general><general>MDPI</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L6V</scope><scope>M7S</scope><scope>PHGZM</scope><scope>PHGZT</scope><scope>PIMPY</scope><scope>PKEHL</scope><scope>PQEST</scope><scope>PQGLB</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>7X8</scope><scope>5PM</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0002-9474-7468</orcidid><orcidid>https://orcid.org/0000-0003-3604-2352</orcidid><orcidid>https://orcid.org/0000-0001-7038-9494</orcidid><orcidid>https://orcid.org/0000-0002-5294-0075</orcidid></search><sort><creationdate>20241030</creationdate><title>Solar Wind Turbulence and Complexity Probed with Rank-Ordered Multifractal Analysis (ROMA)</title><author>Echim, Marius ; Munteanu, Costel ; Voitcu, Gabriel ; Teodorescu, Eliza</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c360t-c9bcc75d3855fc7d2b6ff22e2716c4a0c4fbb4eb034622217c67a62e08de54b13</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Celestial bodies</topic><topic>Charged particles</topic><topic>Complexity</topic><topic>Data analysis</topic><topic>Ecliptic</topic><topic>Energy</topic><topic>Fractal analysis</topic><topic>Fractals</topic><topic>Function analysis</topic><topic>Heliosphere</topic><topic>Hypotheses</topic><topic>intermittency</topic><topic>Magnetic fields</topic><topic>Magnetic variations</topic><topic>multifractal analysis</topic><topic>Plasma</topic><topic>rank-ordered multifractal analysis</topic><topic>River networks</topic><topic>Solar wind</topic><topic>Spacecraft</topic><topic>Turbulence</topic><topic>Venus Express (ESA)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Echim, Marius</creatorcontrib><creatorcontrib>Munteanu, Costel</creatorcontrib><creatorcontrib>Voitcu, Gabriel</creatorcontrib><creatorcontrib>Teodorescu, Eliza</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>Engineering Research Database</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>ProQuest Engineering Collection</collection><collection>ProQuest Engineering Database</collection><collection>ProQuest Central (New)</collection><collection>ProQuest One Academic (New)</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Middle East (New)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Applied & Life Sciences</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Engineering collection</collection><collection>MEDLINE - Academic</collection><collection>PubMed Central (Full Participant titles)</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Entropy (Basel, Switzerland)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Echim, Marius</au><au>Munteanu, Costel</au><au>Voitcu, Gabriel</au><au>Teodorescu, Eliza</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Solar Wind Turbulence and Complexity Probed with Rank-Ordered Multifractal Analysis (ROMA)</atitle><jtitle>Entropy (Basel, Switzerland)</jtitle><addtitle>Entropy (Basel)</addtitle><date>2024-10-30</date><risdate>2024</risdate><volume>26</volume><issue>11</issue><spage>929</spage><pages>929-</pages><issn>1099-4300</issn><eissn>1099-4300</eissn><abstract>The Rank-Ordered Multifractal Analysis (ROMA) is a tool designed to characterize scale (in)variance and multifractality based on rank ordering the fluctuations in "groups" characterized by the same mono-fractal behavior (Hurst exponent). A range-limited structure-function analysis provides the mono-fractal index for each rank-ordered range of fluctuations. We discuss here two examples of multi-scale solar wind turbulence and complexity where ROMA is applied on the following: (a) data collected by Ulysses spacecraft in the fast solar wind, outside the ecliptic, between 25 and 31 January 2007, at roughly 2.5 Astronomical Units (AU) from the Sun, in the Southern heliosphere, at latitudes between -76.5 and -77.3 degrees, and (b) slow solar wind data collected in the ecliptic plane by Venus Express spacecraft, at 0.72 AU, on 28 January 2007. The ROMA spectrum of fast solar wind derived from ULYSSES data shows a scale-dependent structure of fluctuations: (1) at the smallest/kinetic range of scales (800 to 3200 km), persistent fluctuations are dominant, and (2) at the inertial range of scales (10
to 2 × 10
km), anti-persistent fluctuations are dominant, but less clearly developed and possibly indicative for the development of instabilities with cross-over behavior. The ROMA spectrum of the slow solar wind derived from Venus Express data, suggests a different structure of turbulence: (1) fully developed multifractal turbulence across scales between 5 × 10
and 4 × 10
km, with the Hurst index changing from anti-persistent to persistent values for the larger amplitude magnetic fluctuations; (2) at the smallest scales (400 to 6400 km), fluctuations are mainly anti-persistent, and the ROMA spectrum indicates a tendency towards mono-fractal behavior.</abstract><cop>Switzerland</cop><pub>MDPI AG</pub><pmid>39593874</pmid><doi>10.3390/e26110929</doi><orcidid>https://orcid.org/0000-0002-9474-7468</orcidid><orcidid>https://orcid.org/0000-0003-3604-2352</orcidid><orcidid>https://orcid.org/0000-0001-7038-9494</orcidid><orcidid>https://orcid.org/0000-0002-5294-0075</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Celestial bodies Charged particles Complexity Data analysis Ecliptic Energy Fractal analysis Fractals Function analysis Heliosphere Hypotheses intermittency Magnetic fields Magnetic variations multifractal analysis Plasma rank-ordered multifractal analysis River networks Solar wind Spacecraft Turbulence Venus Express (ESA) |
title | Solar Wind Turbulence and Complexity Probed with Rank-Ordered Multifractal Analysis (ROMA) |
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