2 edition of Estimation of flood-frequency characteristics of small urban streams in North Carolina found in the catalog.
Estimation of flood-frequency characteristics of small urban streams in North Carolina
Jeanne C. Robbins
1996 by U.S. Dept. of the Interior, U.S. Geological Survey, Branch of Information Services [distributor] in Raleigh, N.C, Denver, CO .
Written in English
Includes bibliographical references (p. 18-19).
|Statement||by Jeanne C. Robbins and Benjamin F. Pope ; prepared in cooperation with the North Carolina Department of Transportation, and the cities of Asheville, Fayetteville, and Raleigh, North Carolina.|
|Series||Water-resources investigations report ;, 96-4084|
|Contributions||Pope, Benjamin F., North Carolina. Dept. of Transportation.|
|LC Classifications||GB701 .W375 no. 96-4084|
|The Physical Object|
|Pagination||iv, 21 p. :|
|Number of Pages||21|
|LC Control Number||97118475|
Project Summary – RES 10/21/ Problem. Planners and engineers require reliable estimates of the magnitude and frequency of floods to design bridges, culverts, and other structures near unregulated streams and rivers. In order to estimate the magnitude and frequency of floods at ungaged sites reliably, prediction. Unfortunately, this book can't be printed from the OpenBook. If you need to print pages from this book, we recommend downloading it as a PDF. Visit to get more information about this book, to buy it in print, or to download it as a free PDF. 1 percent chance (or year) flood elevation, which is a relatively small flood, especially in urban areas. It has a one in four chance of occurring over a year mortgage. Other developed nations, such as the UK and in Europe tend to have higher standards for development. National flood policy has also changed regarding structural flood File Size: 1MB. Book set: Environmental and Water Resources ISBN (print): Assessment of Urban Streams in Fairmount Park, Philadelphia, PA. Christina Cianfrani, An Approach for Evaluating Flood Frequency Estimates for Ungaged Watersheds. Wilbert O. Thomas, Jr., Michael M. Grimm and Richard H. McCuen.
REGIONAL AND SAMPLE SKEW VALUES IN FLOOD-FREQUENCY ANALYSES OF STREAMS IN ILLINOIS by Krishan P. Singh, Ph.D., P.E. ABSTRACT. Storm, basin, stream, soil, floodplain, and other relevant factors were investigated for 62 basins in areas drained by the Sangamon, Rock, and Little Wabash Rivers in Illinois, to understand the variation in.
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ESTIMATION OF FLOOD-FREQUENCY CHARACTERISTICS OF SMALL URBAN STREAMS IN NORTH CAROLINA By Jeanne C. Robbins and Benjamin F. Pope U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report Prepared in cooperation with the NORTH CAROLINA DEPARTMENT OF TRANSPORTATION, and the CITIES of ASHEVILLE, FAYETTEVILLE, and Cited by: 6.
Get this from a library. Estimation of flood-frequency characteristics of small urban streams in North Carolina. [Jeanne C Robbins; Benjamin F Pope; North Carolina. Department of Transportation.]. Estimation of flood-frequency characteristics of small urban streams in North Carolina Water-Resources Investigations Report By Jeanne C Robbins and Benjamin F Pope III.
The at-site flood-frequency analysis of annual peak-flow data for urban and small, rural streams (through Septem ) included urban streamgages and 32 small, rural streamgages, defined in this report as basins draining less than 1 square mile.
WRIREstimation of Flood-Frequency Characteristics of Small Urban Streams in North Carolina North Dakota SIRRegional regression equations to estimate peak-flow frequency at sites in North Dakota using data through similar approach was applied to urban and small, rural streams (Feaster and others, ).
For this investigation, Southeast refers specifically to Georgia, South Carolina, and North Carolina. The analytical techniques used incorporate both urban and rural streamgages and, therefore, can be applied to urban and small, rural Size: KB. This report provides a method for estimating the magnitude and frequency of floods for small streams in the Philadelphia, Pennsylvania area.
Data collected at 21 streamflow gaging stations were used in a multiple-regression analysis to develop equations for computation of peak-flow characteristics. The flood equations were determined by relating flood-frequency characteristics computed using.
The flood-frequency estimates are particularly important in densely populated urban areas. A multistate approach was used to update methods for determining the magnitude and frequency of floods in urban and small, rural streams that are not substantially affected by regulation or tidal fluctuations in Georgia, South Carolina, and North : Toby D Feaster, Anthony J Gotvald, J Curtis Weaver.
Robbins JC, Pope BF () Estimation of flood frequency characteristics of small urban streams in North Carolina. US Geol Surv Water Resources Inv Rep21 pages Sauer VB () Flood characteristics of urban watersheds in the United by: 3. The results of the project will be documented in a USGS Scientific Investigations Report, tentatively titled “Methods for estimating the magnitude and frequency of floods for urban and small, rural, Piedmont-Ridge and Valley, Sand Hills, and Coastal Plain streams in the Southeastern United States, Georgia, South Carolina, and North.
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.
We examine urban flood response through data-driven analyses for a diverse sample of “small” watersheds (basin scale ranging from to km2) in the Charlotte Metropolitan region.
Comparison of methods for estimation of year peak discharge from a small, rural watershed in North Carolina Article (PDF Available) in Environmental Geology 44(1) May with Reads. A statewide study was conducted to develop two methods for estimating the magnitude and frequency of floods in rural ungaged basins in North Carolina.
Flood-frequency estimates for gaged sites in North Carolina were computed by fitting the annual peak flows for each site to a log. Point of contact for NFF: U.S.
Geological Survey Office of Surface Water Sunrise Valley Dr., MS Reston, VA (electronic mail: [email protected]). : Magnitude and Frequency of Rural Floods in the Southeastern United States, Through Volume 2, North Carolina: Usgs Scientific Investigations Repo Authors: J. Curtis Weaver, Sean E.
Low. urban flood frequency characteristics. this paper presents the results of a study concerning the occurrence and factors effecting floods from small urban watersheds. based on log-pearson type iii flood frequency analysis on four urban watersheds located in texas, urbanization has.
Bohman, L.R.,Determination of flood hydrographs for streams in South Carolina: Volume 2. Estimation of peak-discharge frequency, runoff volumes, and flood hydrographs for urban watersheds: U.S. Geological Survey Water-Resources Investigations Report79 p.
Book/Printed Material Estimating flood-peak discharge magnitudes and frequencies for rural streams in Illinois / About this Item. Title Title Estimating flood-peak discharge magnitudes and frequencies for rural streams in Illinois / Created / Published Peak flow characteristics of Wyoming streams Two folded colored maps in pocket.
The U.S. Geological Survey, in cooperation with the South Carolina Department of Transportation, updated these data from previous flood-frequency reports to aid officials who are active in floodplain management as well as those who design bridges, culverts, and levees, or other structures near streams where flooding is likely to occur.
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: StreamStats Application. StreamStats is a Web application that provides access to an assortment of Geographic Information Systems (GIS) analytical tools that are useful for water-resources planning and management, and for engineering and design purposes.
The map-based user interface can be used to delineate drainage areas for user-selected sites on streams, and then get basin characteristics. • Since small catchments are not well represented in HiFlows-UK, further flood peak data for small rural and urban catchments should be sought and analysed.
• Despite lack of bias, uncertainty in flood estimation remains high and there is a need to develop and test improved catchment descriptors, especially of soils and watercourse extent. Regional Flood Frequency Estimation Model. List of Related Publications.
Stage 1 Report; Stage 2 Report; Stage 3 Report; Haddad K and Rahman A (): Regional flood frequency analysis in eastern Australia: Bayesian GLS regression-based methods within fixed region and ROI framework ‒ Quantile regression vs.
parameter regression technique, Journal of Hydrology,report contains flood data and basin characteristics for urban sites in 56 cities and 31 states.
It also has an extensive list of references for both urban and rural flood-frequency procedures. After analysis of the nationwide regionalization (2), five new urban studies were prepared for cit.
Regional Flood Frequency Estimation Model. Release Version of the Regional Flood Frequency Estimation Model for the 4th edition of Australian Rainfall and Runoff. stations comprise streamgaging stations in Georgia, 82 in South Carolina, in North Carolina, 35 in Alabama, 23 in Florida, 41 in Tennessee, and 72 in Virginia.
Figure 2. Locations of rural streamgaging stations in Georgia, South Carolina, North Carolina, and surrounding States considered for use in the regional regression : South Carolina, Toby Feaster, Anthony Gotvald, Curtis Weaver.
Floods on small streams in North Carolina, probable magnitude and frequency, (Washington, D.C.: [G.P.O.], ), by Herbert G. Hinson and North Carolina State Highway Commission (page images at HathiTrust) Floods of May in southeastern Montana and northeastern Wyoming / ([Reston, Va.?].
Magnitude and Frequency of Floods for Rural, Unregulated Streams of Tennessee by L-Moments Method Hongxiang Yan University of Arkansas, Fayetteville "Magnitude and Frequency of Floods for Rural, Unregulated Streams of Tennessee by L-Moments Method" ().
Theses and Dissertations. THE SELECTED BASIN CHARACTERISTICS AND FLOOD-FREQUENCYCited by: 6. Magnitude and Frequency of Rural Floods in the Southeastern United States, Volume 3, South Carolina. A multistate approach was used to update methods for estimating the magnitude and frequency of floods in rural, ungaged basins in South Carolina, Georgia, and North Carolina that are not substantially affected by regulation, tidal fluctuations, or urban development.
1 NEW REGIONAL FLOOD FREQUENCY ESTIMATION (RFFE) METHOD FOR THE WHOLE OF AUSTRALIA: OVERVIEW OF PROGRESS A. Rahman 1, K. Haddad 1, M.
Zaman, G. Kuczera 2, P. Weinmann 3, P. Stensmyr 4, M. Babister 1School of Computing, Engineering and Mathematics, University of Western Sydney 2School of Engineering, The University of Newcastle 3Department of. As part of the EWRI sponsored World Water and Environmental Resources Congress, June, in Philadelphia, the Urban Streams Technical Committee of the Urban Water Resources Research Council (UWRRC) and the Urban Stream Restoration Technical Committee of the Watershed Council are co-sponsoring an international symposium on the restoration and protection of streams with emphasis.
RESEARCH ARTICLE /WR The complexities of urban flood response: Flood frequency analyses for the Charlotte metropolitan region Zhengzheng Zhou1,2,3, James A. Smith 2, Long Yang 2, Mary Lynn Baeck, Molly Chaney, Marie-Claire Ten Veldhuis4, Huiping Deng3,5, and Shuguang Liu1,3 1Department of Hydraulic Engineering, Tongji University, Shanghai, China, 2Department of Cited by: 7.
Characteristics Affecting Effective Discharge of Small Urban - Streams in Southern Ontario / Asif Quader, Yiping Quo Sensitivity of Conceptual and Physically Based Hydrologic Models to Temporal and Spatial Rainfall Sampling / E.
Meselhe, E. Habib, O. Oche, S. Gautam. Science -- Forecasting. See also what's at your library, or elsewhere. Broader terms: Science; Forecasting; Narrower term: Environmental sciences -- Forecasting; Filed under: Envi.
Ungauged estimation can be obtained either by establishing a regression between catchments characteristics and the mean value of annual maxima, or by performing a direct regression of the at-site T-year event estimate on the catchment by: 3.
The October 3–5, historic rains caused by hurricane Joaquin released more than mm of rain in South Carolina (SC) and North Carolina (NC), United States (US).
The flood peak of many U.S. Geological Survey (USGS) gauges, including those located in the center of SC, were almost twice the previous maximum from a record of over 65 : R.C.
Phillips, S.Z. Samadi, M.E. Meadows. streams or reaches lacking systematic stream gauge data; therefore, estimates of flow duration characteristics and the frequency of extreme high and extreme low flows must be based on indirect methods from regional hydrologic analysis.
Flood Frequency Analysis Guidelines for determining the fre-quency of floods at a particular location. Rahman et al., Features of regional flood frequency estimation model Kx = frequency factor for the LP3 distribution for AEP of x%, which is a function of the AEP and the skewness (SK) of the natural logarithms of the annual maximum flood series Figure 2.
Adopted regions in the ARR RFFE Model Table 3. Regions in arid/semi-arid areas of Size: 1MB. Full text of "Flood flow frequency for ungaged watersheds: a literature evaluation" See other formats. A flood frequency curve is a valuable tool to extrapolate how often a flood of a given discharge will occur.
A flood frequency curve can be constructed by plotting a graph of discharge versus recurrence interval. This can easily be accomplished provided you have a data .small dams in sparsely populated areas. In other engineering examples the appropriate design frequency may be deduced by optimising the balance between expected damage and the cost of damage reduction by flood control.
This requires estimates of the flood frequency relation and the extent of .Channel-forming discharges typically are associated with recurrence intervals less than five years and usually less than two years. However, the actual frequency of occurrence of these discharges is often several times more frequent than the statistical expectation.
This result was confirmed by using the Log-Pearson Type 3 statistical method to analyze measured annual series of instantaneous Cited by: 1.