Item talk:Q326070

{

 "DOI": {
   "doi": "10.5066/p9yuv9dg",
   "identifiers": [],
   "creators": [
     {
       "name": "Domanski, Marian M",
       "nameType": "Personal",
       "givenName": "Marian M",
       "familyName": "Domanski",
       "affiliation": [
         "United States Geological Survey"
       ],
       "nameIdentifiers": []
     },
     {
       "name": "Holmes, Robert R",
       "nameType": "Personal",
       "givenName": "Robert R",
       "familyName": "Holmes",
       "affiliation": [
         "United States Geological Survey"
       ],
       "nameIdentifiers": [
         {
           "schemeUri": "https://orcid.org",
           "nameIdentifier": "https://orcid.org/0000-0002-5060-3999",
           "nameIdentifierScheme": "ORCID"
         }
       ]
     },
     {
       "name": "Heal, Elizabeth N",
       "nameType": "Personal",
       "givenName": "Elizabeth N",
       "familyName": "Heal",
       "affiliation": [],
       "nameIdentifiers": [
         {
           "schemeUri": "https://orcid.org",
           "nameIdentifier": "https://orcid.org/0000-0002-1196-4708",
           "nameIdentifierScheme": "ORCID"
         }
       ]
     }
   ],
   "titles": [
     {
       "title": "Dynamic stage to discharge rating model archive"
     }
   ],
   "publisher": "U.S. Geological Survey",
   "container": {},
   "publicationYear": 2022,
   "subjects": [
     {
       "subject": "Hydrology, Water Resources"
     }
   ],
   "contributors": [],
   "dates": [
     {
       "date": "2022",
       "dateType": "Issued"
     }
   ],
   "language": null,
   "types": {
     "ris": "DATA",
     "bibtex": "misc",
     "citeproc": "dataset",
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     "resourceType": "Dataset",
     "resourceTypeGeneral": "Dataset"
   },
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       "relationType": "IsCitedBy",
       "relatedIdentifier": "10.3133/ofr20221031",
       "relatedIdentifierType": "DOI"
     }
   ],
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   "version": null,
   "rightsList": [],
   "descriptions": [
     {
       "description": "Ratings are used for a variety of reasons in water-resources investigations. The simplest rating relates discharge to the stage of the river. From a pure hydrodynamics perspective, all rivers and streams have some form of hysteresis in the relation between stage and discharge because of unsteady flow as a flood wave passes. Simple ratings are unable to represent hysteresis in a stage/discharge relation. A dynamic rating method is capable of capturing hysteresis owing to the variable energy slope caused by unsteady momentum and pressure. Using some simplifying assumptions, Fread (1973) developed what was termed a \u201cdynamic loop\u201d rating method to compute discharge from a time series of stage at a single streamgage for channels with compact [...]",
       "descriptionType": "Abstract"
     }
   ],
   "geoLocations": [],
   "fundingReferences": [],
   "url": "https://www.sciencebase.gov/catalog/item/61ef284bd34e8b818adb7b75",
   "contentUrl": null,
   "metadataVersion": 2,
   "schemaVersion": "http://datacite.org/schema/kernel-4",
   "source": "mds",
   "isActive": true,
   "state": "findable",
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   "created": "2022-06-07T21:17:46Z",
   "registered": "2022-06-07T21:17:47Z",
   "published": null,
   "updated": "2022-07-24T04:36:57Z"
 }

}