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Revision as of 18:16, 22 August 2024 by Sky (talk | contribs) (Created page with "{ "USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "Conference Paper", "name": "Techniques for estimating sediment yield of ungaged tributaries on the southern Colorado Plateau", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70216719", "url": "https://pubs.usgs.gov/publication/70216719"...")
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{

 "USGS Publications Warehouse": {
   "@context": "https://schema.org",
   "@type": "CreativeWork",
   "additionalType": "Conference Paper",
   "name": "Techniques for estimating sediment yield of ungaged tributaries on the southern Colorado Plateau",
   "identifier": [
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       "@type": "PropertyValue",
       "propertyID": "USGS Publications Warehouse IndexID",
       "value": "70216719",
       "url": "https://pubs.usgs.gov/publication/70216719"
     },
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       "propertyID": "USGS Publications Warehouse Internal ID",
       "value": 70216719
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   ],
   "inLanguage": "en",
   "datePublished": "2001",
   "dateModified": "2020-12-02",
   "abstract": "Numerous regional sediment transport data are used to evaluate three techniques for estimating streamflow sediment yield from ungaged tributaries of the Colorado River in Grand Canyon. These techniques include: (1) a regression equation relating drainage area to sediment yield for all relevant sediment-yield data from northern Arizona, (2) an empirical relation developed by Renard (1972) selected from 8 potentially relevant methods, and (3) a new procedure that combines regional flood-frequency analysis with sediment-rating curves. Results based on techniques (1) and (2) are not significantly different. The third technique requires numerous assumptions, most notably that sediment yield on a decadal average can be described by several floods of recurrence intervals of 2 yr, 5 yr, and 10 yr described by regional flood-frequency relations. Using data collected at gaging stations, we develop a relation between peak discharge and total-event sediment yield derived from hydrographs and sediment-rating curves. This third technique produces sediment yield estimates comparable to those of the regional data regression and Renard (1972) relations and may be a more robust technique for estimating sediment yield when streamflow data are available.",
   "description": "8 p.",
   "publisher": {
     "@type": "Organization",
     "name": "Inter-agency Committee on Water Resources. Subcommittee on Sedimentation"
   },
   "author": [
     {
       "@type": "Person",
       "name": "Webb, Robert rhwebb@usgs.gov",
       "givenName": "Robert",
       "familyName": "Webb",
       "email": "rhwebb@usgs.gov"
     },
     {
       "@type": "Person",
       "name": "Griffiths, Peter G. pggriffi@usgs.gov",
       "givenName": "Peter G.",
       "familyName": "Griffiths",
       "email": "pggriffi@usgs.gov",
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       "@type": "Person",
       "name": "Hartley, Daniel R.",
       "givenName": "Daniel R.",
       "familyName": "Hartley"
     }
   ],
   "funder": [
     {
       "@type": "Organization",
       "name": "Rocky Mountain Regional Office",
       "url": "https://www.usgs.gov/regions/rocky-mountain"
     }
   ],
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       "additionalType": "country",
       "name": "United States",
       "url": "https://geonames.org/4074035"
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       "name": "Arizona"
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       "name": "Colorado River",
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       "name": "Grand Canyon",
       "url": "https://geonames.org/4239673"
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