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Influence of the zero-rainfall on the assessment of the multifractal parameters
► Truncated multifractal fields exhibit a 2nd order phase transition for low moments. ► Universal multifractal exponents’ estimates are affected by truncation of the field. ► The main features of rainfall data are retrieved on truncated simulated fields. ► A new technique to thwart this threshold ef...
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Published in: | Advances in water resources 2012-09, Vol.45, p.13-25 |
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creator | Gires, A. Tchiguirinskaia, I. Schertzer, D. Lovejoy, S. |
description | ► Truncated multifractal fields exhibit a 2nd order phase transition for low moments. ► Universal multifractal exponents’ estimates are affected by truncation of the field. ► The main features of rainfall data are retrieved on truncated simulated fields. ► A new technique to thwart this threshold effect provides encouraging results.
Rainfall data contains numerous zero values, either real or spurious, especially at high resolution. This paper investigates how a truncation of a multifractal field affects the scaling analysis. Synthetic multifractal fields are used. The main result, which is theoretically expected and empirically observed, is that the truncated fields exhibit a multifractal phase transition for small moments. This implies an under-estimation of the multifractality index, and consequently of the extremes. This framework enables one to retrieve most of the features observed on radar data corresponding to a heavy rainfall event that occurred in September 2005 in the South of France. Finally a new technique is proposed to improve the estimation of characteristic multifractal parameters. It yields imperfect but encouraging results. |
doi_str_mv | 10.1016/j.advwatres.2012.03.026 |
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Rainfall data contains numerous zero values, either real or spurious, especially at high resolution. This paper investigates how a truncation of a multifractal field affects the scaling analysis. Synthetic multifractal fields are used. The main result, which is theoretically expected and empirically observed, is that the truncated fields exhibit a multifractal phase transition for small moments. This implies an under-estimation of the multifractality index, and consequently of the extremes. This framework enables one to retrieve most of the features observed on radar data corresponding to a heavy rainfall event that occurred in September 2005 in the South of France. Finally a new technique is proposed to improve the estimation of characteristic multifractal parameters. It yields imperfect but encouraging results.</description><identifier>ISSN: 0309-1708</identifier><identifier>EISSN: 1872-9657</identifier><identifier>DOI: 10.1016/j.advwatres.2012.03.026</identifier><identifier>CODEN: AWREDI</identifier><language>eng</language><publisher>Kidlington: Elsevier Ltd</publisher><subject>Applied geophysics ; Earth sciences ; Earth, ocean, space ; Environmental Sciences ; Exact sciences and technology ; Hydrology ; Hydrology. Hydrogeology ; Internal geophysics ; Multifractal phase transition ; Multifractals ; Scale invariance ; Truncated fields ; Zero rainfall</subject><ispartof>Advances in water resources, 2012-09, Vol.45, p.13-25</ispartof><rights>2012 Elsevier Ltd</rights><rights>2015 INIST-CNRS</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c379t-4febc96fdfb2447fdf7c79a83f571c499993295221e02e9713e460c6936b88ff3</citedby><cites>FETCH-LOGICAL-c379t-4febc96fdfb2447fdf7c79a83f571c499993295221e02e9713e460c6936b88ff3</cites><orcidid>0000-0002-4121-9928 ; 0000-0003-4930-5115</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,309,310,314,776,780,785,786,881,23909,23910,25118,27901,27902</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=26294097$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://enpc.hal.science/hal-00786091$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Gires, A.</creatorcontrib><creatorcontrib>Tchiguirinskaia, I.</creatorcontrib><creatorcontrib>Schertzer, D.</creatorcontrib><creatorcontrib>Lovejoy, S.</creatorcontrib><title>Influence of the zero-rainfall on the assessment of the multifractal parameters</title><title>Advances in water resources</title><description>► Truncated multifractal fields exhibit a 2nd order phase transition for low moments. ► Universal multifractal exponents’ estimates are affected by truncation of the field. ► The main features of rainfall data are retrieved on truncated simulated fields. ► A new technique to thwart this threshold effect provides encouraging results.
Rainfall data contains numerous zero values, either real or spurious, especially at high resolution. This paper investigates how a truncation of a multifractal field affects the scaling analysis. Synthetic multifractal fields are used. The main result, which is theoretically expected and empirically observed, is that the truncated fields exhibit a multifractal phase transition for small moments. This implies an under-estimation of the multifractality index, and consequently of the extremes. This framework enables one to retrieve most of the features observed on radar data corresponding to a heavy rainfall event that occurred in September 2005 in the South of France. Finally a new technique is proposed to improve the estimation of characteristic multifractal parameters. It yields imperfect but encouraging results.</description><subject>Applied geophysics</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Environmental Sciences</subject><subject>Exact sciences and technology</subject><subject>Hydrology</subject><subject>Hydrology. Hydrogeology</subject><subject>Internal geophysics</subject><subject>Multifractal phase transition</subject><subject>Multifractals</subject><subject>Scale invariance</subject><subject>Truncated fields</subject><subject>Zero rainfall</subject><issn>0309-1708</issn><issn>1872-9657</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNqFkE1LAzEQhoMoWKu_wb148LDrJNkmm2MpaguFXvQc0nRCU_ajJNuK_nqzVnt1LgPD884wDyH3FAoKVDztCrM5fpg-YCwYUFYAL4CJCzKilWS5EhN5SUbAQeVUQnVNbmLcAUBVSjYiq0Xr6gO2FrPOZf0Wsy8MXR6Mb52p66xrf4YmRoyxwbb_w5pD3XsXjO1Nne1NMA32GOItuUq5iHe_fUzeX57fZvN8uXpdzKbL3HKp-rx0uLZKuI1bs7KUqUsrlam4m0hqS5WKMzVhjCIwVJJyLAVYobhYV5VzfEweT3u3ptb74BsTPnVnvJ5Pl3qYAchKgKJHmlh5Ym3oYgzozgEKenCod_rsUA8ONXCdHKbkwym5N9GaOr3bWh_PcSaYKkHJxE1PHKaXjx6DjtYPUjc-oO31pvP_3voGrYyMBg</recordid><startdate>20120901</startdate><enddate>20120901</enddate><creator>Gires, A.</creator><creator>Tchiguirinskaia, I.</creator><creator>Schertzer, D.</creator><creator>Lovejoy, S.</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0002-4121-9928</orcidid><orcidid>https://orcid.org/0000-0003-4930-5115</orcidid></search><sort><creationdate>20120901</creationdate><title>Influence of the zero-rainfall on the assessment of the multifractal parameters</title><author>Gires, A. ; Tchiguirinskaia, I. ; Schertzer, D. ; Lovejoy, S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c379t-4febc96fdfb2447fdf7c79a83f571c499993295221e02e9713e460c6936b88ff3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Applied geophysics</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Environmental Sciences</topic><topic>Exact sciences and technology</topic><topic>Hydrology</topic><topic>Hydrology. Hydrogeology</topic><topic>Internal geophysics</topic><topic>Multifractal phase transition</topic><topic>Multifractals</topic><topic>Scale invariance</topic><topic>Truncated fields</topic><topic>Zero rainfall</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gires, A.</creatorcontrib><creatorcontrib>Tchiguirinskaia, I.</creatorcontrib><creatorcontrib>Schertzer, D.</creatorcontrib><creatorcontrib>Lovejoy, S.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Advances in water resources</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gires, A.</au><au>Tchiguirinskaia, I.</au><au>Schertzer, D.</au><au>Lovejoy, S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Influence of the zero-rainfall on the assessment of the multifractal parameters</atitle><jtitle>Advances in water resources</jtitle><date>2012-09-01</date><risdate>2012</risdate><volume>45</volume><spage>13</spage><epage>25</epage><pages>13-25</pages><issn>0309-1708</issn><eissn>1872-9657</eissn><coden>AWREDI</coden><abstract>► Truncated multifractal fields exhibit a 2nd order phase transition for low moments. ► Universal multifractal exponents’ estimates are affected by truncation of the field. ► The main features of rainfall data are retrieved on truncated simulated fields. ► A new technique to thwart this threshold effect provides encouraging results.
Rainfall data contains numerous zero values, either real or spurious, especially at high resolution. This paper investigates how a truncation of a multifractal field affects the scaling analysis. Synthetic multifractal fields are used. The main result, which is theoretically expected and empirically observed, is that the truncated fields exhibit a multifractal phase transition for small moments. This implies an under-estimation of the multifractality index, and consequently of the extremes. This framework enables one to retrieve most of the features observed on radar data corresponding to a heavy rainfall event that occurred in September 2005 in the South of France. Finally a new technique is proposed to improve the estimation of characteristic multifractal parameters. It yields imperfect but encouraging results.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.advwatres.2012.03.026</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-4121-9928</orcidid><orcidid>https://orcid.org/0000-0003-4930-5115</orcidid></addata></record> |
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subjects | Applied geophysics Earth sciences Earth, ocean, space Environmental Sciences Exact sciences and technology Hydrology Hydrology. Hydrogeology Internal geophysics Multifractal phase transition Multifractals Scale invariance Truncated fields Zero rainfall |
title | Influence of the zero-rainfall on the assessment of the multifractal parameters |
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