A physically based watershed partitioning method
A new contour-based watershed partitioning method, relying on tracking flow lines moving from upslope to downslope, is presented. The model works by using only contour data and consists of three principal steps: 1) Ideal Drainage Network tracking; 2) hillslope and channel elements building; and 3) a...
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Veröffentlicht in: | Advances in water resources 2010-10, Vol.33 (10), p.1206-1215 |
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description | A new contour-based watershed partitioning method, relying on tracking flow lines moving from upslope to downslope, is presented. The model works by using only contour data and consists of three principal steps: 1) Ideal Drainage Network tracking; 2) hillslope and channel elements building; and 3) actual contour-based element network construction. It automatically detects and manages sinks, peaks and saddles and calculates element attributes taking into account the non-planar shape of the elements. Watershed, subwatershed and draining area at any point can be automatically detected by using network elements interconnectivity. It is also possible to determine the Actual Drainage Network.
The model is able to manage point data set trough interpolation, according with specific procedures. Also grid datasets can be used as input, the model is in fact provided with an overlapping algorithm for matching grid datasets to elements.
Comparisons with an existing contour-based element network construction method show a better and more physically based description of the element network particularly useful for hydrological and mass movements' analyses. |
doi_str_mv | 10.1016/j.advwatres.2010.06.011 |
format | Article |
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The model is able to manage point data set trough interpolation, according with specific procedures. Also grid datasets can be used as input, the model is in fact provided with an overlapping algorithm for matching grid datasets to elements.
Comparisons with an existing contour-based element network construction method show a better and more physically based description of the element network particularly useful for hydrological and mass movements' analyses.</description><identifier>ISSN: 0309-1708</identifier><identifier>EISSN: 1872-9657</identifier><identifier>DOI: 10.1016/j.advwatres.2010.06.011</identifier><identifier>CODEN: AWREDI</identifier><language>eng</language><publisher>Kidlington: Elsevier Ltd</publisher><subject>Construction ; Contour-based ; DEM ; Drainage ; Earth sciences ; Earth, ocean, space ; Element network ; Exact sciences and technology ; Hydrology. Hydrogeology ; Mathematical models ; Networks ; Partitioning ; Shape ; Tracking ; Watersheds</subject><ispartof>Advances in water resources, 2010-10, Vol.33 (10), p.1206-1215</ispartof><rights>2010 Elsevier Ltd</rights><rights>2015 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c443t-8c50f40191b409ef44e8c868889797c55820c8470556575e9dcc994668ae8523</citedby><cites>FETCH-LOGICAL-c443t-8c50f40191b409ef44e8c868889797c55820c8470556575e9dcc994668ae8523</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0309170810001235$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>309,310,314,776,780,785,786,3537,23909,23910,25118,27901,27902,65306</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=23432747$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Rulli, M. Cristina</creatorcontrib><title>A physically based watershed partitioning method</title><title>Advances in water resources</title><description>A new contour-based watershed partitioning method, relying on tracking flow lines moving from upslope to downslope, is presented. The model works by using only contour data and consists of three principal steps: 1) Ideal Drainage Network tracking; 2) hillslope and channel elements building; and 3) actual contour-based element network construction. It automatically detects and manages sinks, peaks and saddles and calculates element attributes taking into account the non-planar shape of the elements. Watershed, subwatershed and draining area at any point can be automatically detected by using network elements interconnectivity. It is also possible to determine the Actual Drainage Network.
The model is able to manage point data set trough interpolation, according with specific procedures. Also grid datasets can be used as input, the model is in fact provided with an overlapping algorithm for matching grid datasets to elements.
Comparisons with an existing contour-based element network construction method show a better and more physically based description of the element network particularly useful for hydrological and mass movements' analyses.</description><subject>Construction</subject><subject>Contour-based</subject><subject>DEM</subject><subject>Drainage</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Element network</subject><subject>Exact sciences and technology</subject><subject>Hydrology. Hydrogeology</subject><subject>Mathematical models</subject><subject>Networks</subject><subject>Partitioning</subject><subject>Shape</subject><subject>Tracking</subject><subject>Watersheds</subject><issn>0309-1708</issn><issn>1872-9657</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><recordid>eNqFUMtqwzAQFKWFpmm_ob6UnuyubD2PIfQFgV5yF4q8bhQc25WclPx9FRJy7WmXZWZ2Zgh5pFBQoOJlU9h6_2vHgLEoIV1BFEDpFZlQJctcCy6vyQQq0DmVoG7JXYwbAFBMlhMCs2xYH6J3tm0P2cpGrLMkhiGu0zbYMPrR953vvrMtjuu-vic3jW0jPpznlCzfXpfzj3zx9f45ny1yx1g15spxaBhQTVcMNDaMoXJKKKW01NJxrkpwyQJwngxy1LVzWjMhlEXFy2pKnk-yQ-h_dhhHs_XRYdvaDvtdNIpKAULwKiHlCelCH2PAxgzBb204GArm2JDZmEtD5tiQAWFSQ4n5dP5hY8rfBNs5Hy_0smJVKZlMuNkJhynv3mMw0XnsHNY-oBtN3ft_f_0Bi1J-5w</recordid><startdate>20101001</startdate><enddate>20101001</enddate><creator>Rulli, M. Cristina</creator><general>Elsevier Ltd</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>20101001</creationdate><title>A physically based watershed partitioning method</title><author>Rulli, M. Cristina</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c443t-8c50f40191b409ef44e8c868889797c55820c8470556575e9dcc994668ae8523</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>Construction</topic><topic>Contour-based</topic><topic>DEM</topic><topic>Drainage</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Element network</topic><topic>Exact sciences and technology</topic><topic>Hydrology. Hydrogeology</topic><topic>Mathematical models</topic><topic>Networks</topic><topic>Partitioning</topic><topic>Shape</topic><topic>Tracking</topic><topic>Watersheds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rulli, M. Cristina</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Advances in water resources</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rulli, M. Cristina</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A physically based watershed partitioning method</atitle><jtitle>Advances in water resources</jtitle><date>2010-10-01</date><risdate>2010</risdate><volume>33</volume><issue>10</issue><spage>1206</spage><epage>1215</epage><pages>1206-1215</pages><issn>0309-1708</issn><eissn>1872-9657</eissn><coden>AWREDI</coden><abstract>A new contour-based watershed partitioning method, relying on tracking flow lines moving from upslope to downslope, is presented. The model works by using only contour data and consists of three principal steps: 1) Ideal Drainage Network tracking; 2) hillslope and channel elements building; and 3) actual contour-based element network construction. It automatically detects and manages sinks, peaks and saddles and calculates element attributes taking into account the non-planar shape of the elements. Watershed, subwatershed and draining area at any point can be automatically detected by using network elements interconnectivity. It is also possible to determine the Actual Drainage Network.
The model is able to manage point data set trough interpolation, according with specific procedures. Also grid datasets can be used as input, the model is in fact provided with an overlapping algorithm for matching grid datasets to elements.
Comparisons with an existing contour-based element network construction method show a better and more physically based description of the element network particularly useful for hydrological and mass movements' analyses.</abstract><cop>Kidlington</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.advwatres.2010.06.011</doi><tpages>10</tpages></addata></record> |
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subjects | Construction Contour-based DEM Drainage Earth sciences Earth, ocean, space Element network Exact sciences and technology Hydrology. Hydrogeology Mathematical models Networks Partitioning Shape Tracking Watersheds |
title | A physically based watershed partitioning method |
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