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Regional rainfall intensity formulas based on scaling property of rainfall
This work developed regional Intensity–Duration–Frequency (IDF) formulas for non-recording sites based on the scaling theory. Forty-six recording raingauges over northern Taiwan provide the data set for analysis. The temporal scaling properties of annual maximum rainfall series for various durations...
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Published in: | Journal of hydrology (Amsterdam) 2004-08, Vol.295 (1), p.108-123 |
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container_title | Journal of hydrology (Amsterdam) |
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creator | Yu, Pao-Shan Yang, Tao-Chang Lin, Chin-Sheng |
description | This work developed regional Intensity–Duration–Frequency (IDF) formulas for non-recording sites based on the scaling theory. Forty-six recording raingauges over northern Taiwan provide the data set for analysis. The temporal scaling properties of annual maximum rainfall series for various durations were first investigated. The hypothesis of piecewise simple scaling combined with Gumbel distribution was used to develop the IDF scaling formulas. Since most of parameters in IDF scaling formulas can be estimated from the annual 1-day maximum series, these parameters were regionalized based on the relationship between the scaling exponent and the average of annual 1-day maximum rainfall. Three scaling homogeneous regions were classified by different scaling regimes and regional IDF scaling formulas were developed in each region. The analyzed results reveal that the regional IDF scaling formulas proposed herein resulted in reasonable simulations and verifications. |
doi_str_mv | 10.1016/j.jhydrol.2004.03.003 |
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Forty-six recording raingauges over northern Taiwan provide the data set for analysis. The temporal scaling properties of annual maximum rainfall series for various durations were first investigated. The hypothesis of piecewise simple scaling combined with Gumbel distribution was used to develop the IDF scaling formulas. Since most of parameters in IDF scaling formulas can be estimated from the annual 1-day maximum series, these parameters were regionalized based on the relationship between the scaling exponent and the average of annual 1-day maximum rainfall. Three scaling homogeneous regions were classified by different scaling regimes and regional IDF scaling formulas were developed in each region. The analyzed results reveal that the regional IDF scaling formulas proposed herein resulted in reasonable simulations and verifications.</description><identifier>ISSN: 0022-1694</identifier><identifier>EISSN: 1879-2707</identifier><identifier>DOI: 10.1016/j.jhydrol.2004.03.003</identifier><identifier>CODEN: JHYDA7</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; geographical variation ; Homogeneous regions ; Hydrology ; Hydrology. Hydrogeology ; Intensit-Duration-Frequency formulas ; mathematics and statistics ; meteorological data ; Non-recording sites ; rain ; Rainfall intensity formulas ; Regional analysis ; Scaling theory</subject><ispartof>Journal of hydrology (Amsterdam), 2004-08, Vol.295 (1), p.108-123</ispartof><rights>2004 Elsevier B.V.</rights><rights>2004 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a446t-190341aa5e9dc82f7f5ae220235236e0664afb5cb02397790e7ef50413433da63</citedby><cites>FETCH-LOGICAL-a446t-190341aa5e9dc82f7f5ae220235236e0664afb5cb02397790e7ef50413433da63</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,786,790,27957,27958</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=15949258$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Yu, Pao-Shan</creatorcontrib><creatorcontrib>Yang, Tao-Chang</creatorcontrib><creatorcontrib>Lin, Chin-Sheng</creatorcontrib><title>Regional rainfall intensity formulas based on scaling property of rainfall</title><title>Journal of hydrology (Amsterdam)</title><description>This work developed regional Intensity–Duration–Frequency (IDF) formulas for non-recording sites based on the scaling theory. Forty-six recording raingauges over northern Taiwan provide the data set for analysis. The temporal scaling properties of annual maximum rainfall series for various durations were first investigated. The hypothesis of piecewise simple scaling combined with Gumbel distribution was used to develop the IDF scaling formulas. Since most of parameters in IDF scaling formulas can be estimated from the annual 1-day maximum series, these parameters were regionalized based on the relationship between the scaling exponent and the average of annual 1-day maximum rainfall. Three scaling homogeneous regions were classified by different scaling regimes and regional IDF scaling formulas were developed in each region. The analyzed results reveal that the regional IDF scaling formulas proposed herein resulted in reasonable simulations and verifications.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>geographical variation</subject><subject>Homogeneous regions</subject><subject>Hydrology</subject><subject>Hydrology. Hydrogeology</subject><subject>Intensit-Duration-Frequency formulas</subject><subject>mathematics and statistics</subject><subject>meteorological data</subject><subject>Non-recording sites</subject><subject>rain</subject><subject>Rainfall intensity formulas</subject><subject>Regional analysis</subject><subject>Scaling theory</subject><issn>0022-1694</issn><issn>1879-2707</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><recordid>eNqFkE2LFDEQhoMoOI7-BLEveuveylencxJZ_FoWBHXPoSZdGTP0dMakR5h_b4YZ9Lh1KSieqnp5GHvNoePA-5tdt_t1GnOaOgGgOpAdgHzCVnwwthUGzFO2AhCi5b1Vz9mLUnZQS0q1YnffaRvTjFOTMc4Bp6mJ80JzicupCSnvjxOWZoOFxibNTfE4xXnbHHI6UK5ICv8WX7JntRV6de1r9vDp48_bL-39t89fbz_ct6hUv7TcglQcUZMd_SCCCRpJCBBSC9kT9L3CsNF-UyfWGAtkKGhQXCopR-zlmr273K0hfh-pLG4fi6dpwpnSsTgxSAPaqEdBbgyofhAV1BfQ51RKpuAOOe4xnxwHd1bsdu6q2J0VO5Du7G_N3l4f4FlMyDj7WP4va6us0EPl3ly4gMnhNlfm4YcALgHsoK3klXh_IaiK-xMpu-IjzZ7GmMkvbkzxkSx_AdcOnT8</recordid><startdate>20040810</startdate><enddate>20040810</enddate><creator>Yu, Pao-Shan</creator><creator>Yang, Tao-Chang</creator><creator>Lin, Chin-Sheng</creator><general>Elsevier B.V</general><general>Elsevier Science</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20040810</creationdate><title>Regional rainfall intensity formulas based on scaling property of rainfall</title><author>Yu, Pao-Shan ; Yang, Tao-Chang ; Lin, Chin-Sheng</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a446t-190341aa5e9dc82f7f5ae220235236e0664afb5cb02397790e7ef50413433da63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>geographical variation</topic><topic>Homogeneous regions</topic><topic>Hydrology</topic><topic>Hydrology. Hydrogeology</topic><topic>Intensit-Duration-Frequency formulas</topic><topic>mathematics and statistics</topic><topic>meteorological data</topic><topic>Non-recording sites</topic><topic>rain</topic><topic>Rainfall intensity formulas</topic><topic>Regional analysis</topic><topic>Scaling theory</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yu, Pao-Shan</creatorcontrib><creatorcontrib>Yang, Tao-Chang</creatorcontrib><creatorcontrib>Lin, Chin-Sheng</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Journal of hydrology (Amsterdam)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yu, Pao-Shan</au><au>Yang, Tao-Chang</au><au>Lin, Chin-Sheng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Regional rainfall intensity formulas based on scaling property of rainfall</atitle><jtitle>Journal of hydrology (Amsterdam)</jtitle><date>2004-08-10</date><risdate>2004</risdate><volume>295</volume><issue>1</issue><spage>108</spage><epage>123</epage><pages>108-123</pages><issn>0022-1694</issn><eissn>1879-2707</eissn><coden>JHYDA7</coden><notes>ObjectType-Article-1</notes><notes>SourceType-Scholarly Journals-1</notes><notes>ObjectType-Feature-2</notes><notes>content type line 23</notes><notes>ObjectType-Article-2</notes><notes>ObjectType-Feature-1</notes><abstract>This work developed regional Intensity–Duration–Frequency (IDF) formulas for non-recording sites based on the scaling theory. Forty-six recording raingauges over northern Taiwan provide the data set for analysis. The temporal scaling properties of annual maximum rainfall series for various durations were first investigated. The hypothesis of piecewise simple scaling combined with Gumbel distribution was used to develop the IDF scaling formulas. Since most of parameters in IDF scaling formulas can be estimated from the annual 1-day maximum series, these parameters were regionalized based on the relationship between the scaling exponent and the average of annual 1-day maximum rainfall. Three scaling homogeneous regions were classified by different scaling regimes and regional IDF scaling formulas were developed in each region. The analyzed results reveal that the regional IDF scaling formulas proposed herein resulted in reasonable simulations and verifications.</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><doi>10.1016/j.jhydrol.2004.03.003</doi><tpages>16</tpages></addata></record> |
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subjects | Earth sciences Earth, ocean, space Exact sciences and technology geographical variation Homogeneous regions Hydrology Hydrology. Hydrogeology Intensit-Duration-Frequency formulas mathematics and statistics meteorological data Non-recording sites rain Rainfall intensity formulas Regional analysis Scaling theory |
title | Regional rainfall intensity formulas based on scaling property of rainfall |
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