Bibliography: p. 27-29.
|Statement||by Marion S. Hines ; prepared by the U.S. Geological Survey in cooperation with the Arkansas Geological Commission.|
|Series||Water resources circular ; no. 12|
|Contributions||Geological Survey (U.S.), Arkansas Geological Commission.|
|LC Classifications||GB705.A8 A23 no. 12, GB1225.A8 A23 no. 12|
|The Physical Object|
|Pagination||v, 75 p. :|
|Number of Pages||75|
|LC Control Number||76621109|
Hines, M. S., , Flow-duration and low-flow frequency determinations of selected Arkansas Streams: Arkansas Geological Commission, Water Resources Circular No. 12, 75 p. 24 Low-Flow Frequency and Flow-Duration Characteristics of Selected Streams in Alabama Through March The assessment showed that the 7Q10 varied from a high of 73 cubic feet per second (ft 3/s) to a low of 50 ft/s, which is a difference of 37 percent. The 7Q10 for the complete period of record was 52 ft3/ by: 1. Buy Flow-duration and low-flow frequency determinations of selected Arkansas streams (Water resources circular ; no. 12) by Marion S Hines (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Marion S Hines. 2 Flow Durations, Low-Flow Frequencies, and Monthly Median Flows for Selected Streams in Connecticut through Locations of streamgaging stations and partial-record sites used in this study are shown on figure 1. This report provides streamflow estimates for 91 con-tinuous-record streamflow-gaging stations with 10 or moreFile Size: 3MB.
The procedure for deriving the long-term flow duration curve at an ungauged site utilises the estimate of natural long-term annual Q95 (as described above) to select a flow duration curve from a family of type curves (standardised by the mean flow).Cited by: The study examined the characteristics of the Sumanpa stream’s Flow-Duration-Frequency Curve statistics for a period of 25years () and compared the . Flow durations, low-flow frequencies, and monthly median streamflows were computed for 91 continuous-record, streamflow-gaging stations in Connecticut with 10 or more years of record. Flow durations include the , , , , , , , , , , , , , , , , 5-, and 1-percent exceedances. Low-flow frequencies include the 7-day, year (7Q10) low flow; 7-day, 2. (–VI–NEH, August ) 5–iii Part National Engineering Handbook Chapter 5 Stream Hydrology Figure 5–7 yr discharges for the Rock Creek watershed in 5–33 Montgomery County, MD Figure 5–8 Typical flow-duration curve 5–38 Figure 5–9 Five basic submodels of a rainfall/runoff model 5–41 Figure 5–10 Bankfull discharge as a function of drainage area for 5–
Low-flow statistics are presented for 18 streamgaging stations in the Pee Dee River basin. In addition, daily flow durations for the 5-, , , , , , and percent probability of exceedance also are presented for the stations. The low-flow characteristics were . Storage Requirements for Arkansas Streams: WRC Floods in Arkansas, Magnitude and Frequency Characteristics through WRC Flow-Duration and Low-Flow Frequency Determinations of Selected Arkansas Streams: WRC Alluvial Aquifer of the Cache and St. Francis River Basins, Northeastern, Arkansas: WRC WRIR , Flow duration and low-flow characteristics of selected Arkansas streams WRIR , Floodflow Frequency of Streams in the Alluvial Plain of the Lower Mississippi River in Mississippi, Arkansas, and Louisiana. Books to Borrow. Top American Libraries Canadian Libraries Universal Library Community Texts Project Gutenberg Biodiversity Heritage Library Children's Library. Open Library. Books by Language Additional Collections. Featured Full text of "Low-flow frequency analysis of streams in New York".