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<br />r,n,'''-,'' <br />II un.l (, <br /> <br />32.2 <br /> <br />WATER INFORMATION MANAGEMENT SYSTEM HANDBOOK <br /> <br />~11 - Method DescriotioDS <br /> <br />~2.11~ - Method A. Method A requires the collection of field <br />data and' use of existing gaging station data. Visit all sites <br />(stations and points of quantification) and measure channel <br />cross sectional area and water surface slope. Method A requires <br />substantial time and effort. <br /> <br />~2.11b - ~~. Method B also requires field visits to all <br />points of quantification, but it entails somewhat less time and <br />effort than Method A. Measure only ~hannel top width 'at bankfull <br />stage in the field. <br /> <br />~2.11c - Method C. Method C requires the use of data that <br />exists or can be developed from gaging station records, maps, <br />photos, and similar sources and some visits to gaging stations <br />for limited data collection. This method utilizes a relation- <br />ship of basin characteristics to bankfull discharge. The <br />relationship(s) is either developed locally or taken from United <br />States Department of Interior (USDI) Geological Surveyor State <br />reports. Examples of basin characteristics include area, <br />precipitation, and mean or area-weighted elevation. <br /> <br />~2.'11d - Method D. Method D requires the use of data that <br />exists or can be developed from gaging station records, maps, <br />photos, and similar sources. Method D does not require field <br />visits although some field verification is desirable. This <br />method utilizes a relationship .between the log-Pearson type III <br />peak flow, for the return interval most nearly equal to the <br />return interval for the selected gage station bankfull <br />discharge, and the watershed area or other appropriate basin <br />characteristics. With the relationship developed, watershed <br />area or other basin characteristics above the point of quanti- <br />fication are used to directly calculate a log-Pearson type III <br />peak flow approximately equivalent to bankfull discharge. <br /> <br />~2.11e - Method E. Apply Method E to those channel reaches <br />which do not adjust their dimension in response to changes in <br />frequent flows. An abbreviated flow requirement is developed <br />which eliminates certain portions of the calculated channel <br />maintenance hydrograph. <br /> <br />~ - Station Selection. All five analysis methods use certain <br />basic relations to calculate bankfull discharge at the.ungaged <br />point(s) of quantification. These relations are developed from <br />the available gaging station data. Gaging stations used in this <br />procedure will most commonly be operated by the United States <br /> <br />*-FSH 4/89 AMEND 3-* <br />