3 edition of Technique for estimating magnitude and frequency of floods in Kentucky found in the catalog.
Technique for estimating magnitude and frequency of floods in Kentucky
C. H. Hannum
by National Technical Information Service, U.S. Dept. of Commerce in Springfield, Va
Written in English
|Statement||by Curtis H. Hannum ; prepared in cooperation with the University of Kentucky, Kentucky Geological Survey, Wallace W. Hagan, Director and State Geologist, November 1976.|
|Series||Water-resources investigations -- 76-62.|
|Contributions||Geological Survey (U.S.). Water Resources Division., Kentucky Geological Survey.|
|The Physical Object|
|Pagination||vi, 74 p. :|
|Number of Pages||74|
Discover our full range of books, gifts, toys, stationery and audiobooks at Buy online with Free UK Delivery on Orders Over £ The National Flood-Frequency Program methods for estimating flood magnitude and frequency in rural and urban areas in North Carolina, / Published: () Techniques for estimating magnitude and frequency of floods in Minnesota / by: Guetzkow, Lowell C., Published: ().
Magnitude and Frequency of Floods for Urban and Small Rural Streams in Georgia, USGS Scientific Investigations Report [Anthony J. Gotvald, Andrew E. Knaak] on *FREE* shipping on qualifying offers. A study was conducted that updated methods for estimating the magnitude and frequency of floods in ungaged urban basins in Georgia that are not substantially . Buy Methods for Estimating Magnitude and Frequency of Floods in the Southwestern United States (U.S. Geological Survey Water-Supply Paper, ) on Cited by:
Hydrology Training Series. Module D - Peak Discharge (Other Methods) Study Guide. US Geological Survey has deve loped techniques for estimating the magnitude and frequency of floods in each state and various to determine the magnitude and frequency of floods at individual. Curtis, G.W., , Technique for estimating flood-peak discharges and frequencies on rural streams in Illinois: U.S. Geological Survey Water-Resources Investigations Report , 79 p. Figure 1. Flood-frequency region map for Illinois. (PostScript file of Figure 1.) Figure 2. The 2 .
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Flood magnitude and frequency relations applicable to unregulated stream in Kentucky are based on flood data at gaging stations in Kentucky and 14.
Technique for estimating magnitude and frequency of floods in Kentucky. Springfield, Va.: National Technical Information Service, U.S.
Dept. of Commerce, [?] (OCoLC) Equations that relate flood magnitude and frequency to contributing drainage area in 16 geographic areas may be used to estimate magnitude of future floods with recurrence intervals of as much as years on gaged and ungaged streams having drainage areas of 10 to 4, square miles ( to 11, square kilometers).
Equations were developed for predicting the magnitude of floods with recurrence intervals of 2, 5, 10, 25, 50, and years in each of the six regions. These equations are applicable to unregulated rural streams with drainage basins ranging in area from square.
This report presents "a technique for estimating the magnitude and frequency of floods in the Houston, Texas, metropolitan area." It includes a map, graph, and by: 9. Abstract. A technique for estimating the magnitude and frequency of floods in the Houston, Texas, metropolitan area was developed by use of a multiple-regression flood-frequency analysis of flow data from unregulated streams in the area.
A regression model, relating flood-peak discharge to concurrent rainfall and antecedent soil moisture conditions, was used to simulate year records of. A technique is presented to provide a method of estimating the magnitude of peak discharges of T-year frequencies for unregulated, virtually natural streams in West Virginia.
Multiple regression techniques were used to develop the relation between peak discharges and drainage area. Data collected at stream gaging sites were used in the analyses. A reliable estimate of the magnitude and frequency of floods is essential to the efficient design of bridges, cul verts, dams, and other hydraulic structures.
In more recent years, the need for flow-frequency estimates has greatly expand ed through implementation of the State Flood Plain Management program and the Federal Flood Insurance by: 9.
TECHNIQUE FOR ESTIMATING MAGNITUDE AND FREQUENCY OF FLOODS ON NATURAL-FLOW STREAMS IN FLORIDA By Wayne C. Bridges ABSTRACT A technique is provided for estimating floods on natural-flow streams in Florida for specific recurrence intervals of 2, 5, 10, 25, 50, and years.
Flood peaks from stream-gaging stations with long-terrrCited by: istics, and the results from a rainfall-runoff model to provide improved flood estimating techniques. Annual peak data from gaging stations (including crest-stage gages and 78 long-term gaging stations) with at least 10 years of record were included in an analysis to develop regional flood-frequency equations for by: Buy Techniques for Estimating Magnitude and Frequency of Floods in the Dallas - Fort Worth Metropolitan Area, Texas (Water - Resources Investigations, ) on FREE SHIPPING on qualified orders.
Information is presented for estimating the magnitude and frequency of floods on streams in South Carolina. Flood-frequency characteristics for gaging stations were related to basin characteristics by multiple regression techniques for each of four physiographic provinces.
Equations were derived to estimate flood magnitudes at recurrence intervals ranging from 2 to years on Cited by: Techniques for estimating magnitude and frequency of floods for Wisconsin streams / Duane H. Conger ; prepared in cooperation with the Wisconsin Department of Transportation ; [prepared by United States Department of the Interior, Geological Survey] The Survey Madison, Wis Australian/Harvard Citation.
Conger, Duane H. & Geological Survey. Techniques for Estimating Magnitude and Frequency of Floods for Urban and Small, Rural Basins in the Southeastern United States, Project Number: GC11MK00CH Project Chief: Toby Feaster Cooperator: South Carolina Department of Transportation Period of Project: May 3, to Decem THIS PROJECT HAS BEEN COMPLETED AND IS BEING ARCHIVED.
A reasonable estimate of the magnitude and frequency of occurrence of peak discharges is required for proper design of structures on the flood plain of a by: Semu Ayalew Moges, Meron Teferi Taye, in Extreme Hydrology and Climate Variability, Introduction. Flood frequency analysis is a technique commonly used to relate the magnitude of extreme runoff or river flow events to their frequency of occurrence through the use of probability distribution functions.
Historical records provide essential information to predict the recurrence. Techniques for estimating magnitude and frequency of floods in South Carolina, (OCoLC) Material Type: Government publication, National government publication, Internet resource: Document Type: Book, Internet Resource: All Authors / Contributors: Wladmir B.
WRIREstimating the Magnitude of Peak Flows for Streams in Kentucky for Selected Recurrence Intervals. WRIREstimating Mean Annual Streamflow of Rural Streams in Kentucky.
WRIREstimation of Peak-Discharge Frequency of Urban Streams in Jefferson County, Kentucky. Techniques for estimating the magnitude and frequency of floods in the Dallas-Fort Worth metropolitan area, Texas (OCoLC) Material Type: Document, Government publication, National government publication, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors.
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Get this from a library! Techniques for estimating the magnitude and frequency of floods in the Houston, Texas, metropolitan area. [Fred Liscum; B C Massey; Houston (Tex.)].This report provides techniques and procedures for estimating the probable magnitude and frequency of floods at ungaged sites on Iowa streams.
Physiographic characteristics were used to define the boundaries of five hydrologic regions. Regional regression equations that relate the size of the drainage area to flood magnitude are defined for estimating peak discharges having specified.technique for estimating magnitude and frequency of floods in tennessee Information is presented for estimating the magnitude and frequency of floods on natural streams in Tennessee.
Flood-frequency characteristics are defined for gaging stations in Tennessee and adjoining states having 10 or more years of record not significantly affected.