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= Annual and approximately quarterly series peak streamflow derived from interpretations of indirect measurements for a crest-stage gage network in Texas through water year 2015 =
{"@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Annual and approximately quarterly series peak streamflow derived from interpretations of indirect measurements for a crest-stage gage network in Texas through water year 2015", "identifier": [{"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "sir20185107", "url": "https://pubs.usgs.gov/publication/sir20185107"}, {"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70198571}, {"@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/sir20185107", "url": "https://doi.org/10.3133/sir20185107"}], "inLanguage": "en", "isPartOf": [{"@type": "CreativeWorkSeries", "name": "Scientific Investigations Report"}], "datePublished": "2018", "dateModified": "2018-09-20", "abstract": "In 2006, the U.S. Geological Survey (USGS), incooperation with the Texas Department of Transportation,began collecting annual and approximately quarterly seriespeak-streamflow data at streamflow-gaging stations in smalltomedium-sized watersheds in central and western Texasas part of a crest-stage gage (CSG) network, along withselected flood-hydrograph data at a subset of these stations.CSGs record the peak stage during storm events, which isthe maximum gage height (elevation of water surface abovea local vertical datum), at each CSG station. Established andwidely used indirect methods of peak streamflow estimationand interpretation, such as culvert-flow, slope-area, andflow-over-road methods, are used in conjunction with peakgage height data to create the database of peak streamflowdescribed herein. The CSG network is focused on hydrologyof small- to medium-sized watersheds in central and westernTexas because additional streamflow data for this semiaridto arid study area will eventually provide for more statisticalinformation and presumably reduced uncertainty in regionalregression equations or other regionalized statistical methodsfor peak-streamflow frequency estimation at ungagedlocations. The database of annual and approximately quarterlypeak streamflow is published through USGS ScienceBase anddescribed in this report.", "description": "Report: vi, 24 p.; Data Release", "publisher": {"@type": "Organization", "name": "U.S. Geological Survey"}, "author": [{"@type": "Person", "name": "Asquith, William H. wasquith@usgs.gov", "givenName": "William H.", "familyName": "Asquith", "email": "wasquith@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-7400-1861", "url": "https://orcid.org/0000-0002-7400-1861"}, "affiliation": [{"@type": "Organization", "name": "Texas Water Science Center", "url": "https://www.usgs.gov/centers/oklahoma-texas-water-science-center"}, {"@type": "Organization", "name": "Lower Mississippi-Gulf Water Science Center", "url": "https://www.usgs.gov/centers/lower-mississippi-gulf-water-science-center"}]}, {"@type": "Person", "name": "Harwell, Glenn R.", "givenName": "Glenn R.", "familyName": "Harwell", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0003-4265-2296", "url": "https://orcid.org/0000-0003-4265-2296"}, "affiliation": [{"@type": "Organization", "name": "Texas Water Science Center", "url": "https://www.usgs.gov/centers/oklahoma-texas-water-science-center"}]}, {"@type": "Person", "name": "Winters, Karl E.", "givenName": "Karl E.", "familyName": "Winters", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-6258-5505", "url": "https://orcid.org/0000-0002-6258-5505"}, "affiliation": [{"@type": "Organization", "name": "Texas Water Science Center", "url": "https://www.usgs.gov/centers/oklahoma-texas-water-science-center"}]}], "funder": [{"@type": "Organization", "name": "Texas Water Science Center", "url": "https://www.usgs.gov/centers/oklahoma-texas-water-science-center"}], "spatialCoverage": [{"@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/6252001"}, {"@type": "Place", "additionalType": "state", "name": "Texas", "url": "https://geonames.org/4736286"}, {"@type": "Place", "geo": [{"@type": "GeoShape", "additionalProperty": {"@type": "PropertyValue", "name": "GeoJSON", "value": {"type": "FeatureCollection", "features": [{"type": "Feature", "properties": {}, "geometry": {"type": "Polygon", "coordinates": [[[-106.0447, 29.785], [-98.566899999999, 29.785], [-98.566899999999, 36.4028], [-106.0447, 36.4028], [-106.0447, 29.785]]]}}]}}}, {"@type": "GeoCoordinates", "latitude": 33.093900000000005, "longitude": -102.3057999999995}]}]}
In 2006, the U.S. Geological Survey (USGS), in<br />
cooperation with the Texas Department of Transportation,<br />
began collecting annual and approximately quarterly series<br />
peak-streamflow data at streamflow-gaging stations in smallto<br />
medium-sized watersheds in central and western Texas<br />
as part of a crest-stage gage (CSG) network, along with<br />
selected flood-hydrograph data at a subset of these stations.<br />
CSGs record the peak stage during storm events, which is<br />
the maximum gage height (elevation of water surface above<br />
a local vertical datum), at each CSG station. Established and<br />
widely used indirect methods of peak streamflow estimation<br />
and interpretation, such as culvert-flow, slope-area, and<br />
flow-over-road methods, are used in conjunction with peak<br />
gage height data to create the database of peak streamflow<br />
described herein. The CSG network is focused on hydrology<br />
of small- to medium-sized watersheds in central and western<br />
Texas because additional streamflow data for this semiarid<br />
to arid study area will eventually provide for more statistical<br />
information and presumably reduced uncertainty in regional<br />
regression equations or other regionalized statistical methods<br />
for peak-streamflow frequency estimation at ungaged<br />
locations. The database of annual and approximately quarterly<br />
peak streamflow is published through USGS ScienceBase and<br />
described in this report.
 
== Table of Contents ==
* Abstract
* Introduction
* Computational Methods for Indirect Measurement of Peak Streamflow
* Annual and Approximately Quarterly Series Peak Streamflow From Interpretations of Indirect Measurements Through Water Year 2015
* Summary
* References Cited

Revision as of 19:37, 15 July 2024

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