Download PDF by Thomas A. McMahon, Russel G. Mein: Reservoir Capacity and Yield

By Thomas A. McMahon, Russel G. Mein

ISBN-10: 0444416692

ISBN-13: 9780444416698

ISBN-10: 0444416706

ISBN-13: 9780444416704

Methodological strategies of the idea of estimation of statistical parameters of time sequence and their software to hydrology and water engineering, really the sector of reservoir-controlled runoffs, are handled during this quantity. For estimates use is made up of random sequences generated for varied chance homes. This methodological technique allows exam of the homes of random and systematic error of the parameters predicted even for the asymmetrical chance distributions, that are widespread in hydrology and water engineering. This ebook should be of curiosity to stochastic hydrologists.

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3 corresponding to z P :>... 57 (Appendix E). 1. 68. 68 x 1274) 866 (x 10 6m3). 06 (Appendix E) is obtained from Fig. 06. 866 x 1. 06 Required storage 920 (x 10 6m3). 5 Carryover Frequency Mass Curve Analysis Carryover frequency analysis is generally similar to the previous techniques. Instead of using theoretical distributions like the Gamma dis- tribution the inflow probability is defined by empirical procedures. of these are now discussed. Two In both of them, the strearnflows are ranked; in the first, overlapping sequences are adopted while independent sequences are used in the other approach.

Concepts are illustrated in Fig. 16. These To obtain a relative measure of severity, commonly rankings are translated into recurrence intervals (return periods) or probabilities, using Eq. 31 . , "C 2 ""E'" Cl ~ o ;;:: Tim e (months) ~ ~ ~ ~ ~ . FIG. 16 ~ Ranked 4 monthly sub - sequences from total sequence of 24 months Rank and sub-sequence concepts (for a 4-monthly sub-sequence, the lowest consecutive four months of flow are ranked as no. 1).

7. In developing his general solution to the storage-yield problem, Hurst computed than mean K and the storage size to "guarantee" a uniform draft x Bless using a mass curve analysis for records of natural phenomena. 96 [(x_B)/S)2 C/R C required reservoir capacity, R range given by Eq. 6) 1. 05 (x-B)/s s draft parameter which is defined x-B s standard deviation of flow, and x mean flow. 7) as draft (3. S) Examining these relationships using only Hurst's river flow data, Joy (1970) found that the generalized curves were not lines of best fit and that the results exhibited large scatter as shown in Fig.

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