| 000 | 00000nam 2200000za 4500 |
| 001 | 9.863052 |
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| 003 | CaOODSP |
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| 005 | 20241203113644 |
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| 007 | cr ||||||||||| |
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| 008 | 181011t19811982oncd #ob f000 0 eng d |
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| 020 | |z0-662-12033-7 |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn-on |
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| 086 | 1 |aEn36-503/122E-PDF|zEn36-503/122E |
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| 100 | 1 |aSangal, B. P., |d1929- |
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| 245 | 12|aA practical method of estimating peak from mean daily flows with application to streams in Ontario |h[electronic resource] / |cB.P. Sangal. |
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| 260 | |aOttawa : |bEnvironment Canada, National Hydrology Research Institute, Inland Waters Directorate, |c1981, c1982. |
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| 300 | |avii, 242 p. : |bgraphs |
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| 490 | 1 |aIWD technical bulletin ; |vno. 122 |
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| 490 | 0 |aNHRI paper ; |vno. 16 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 504 | |aIncludes bibliographical references. |
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| 520 | |a"A practical method has been suggested for estimating peak flow. The method uses variables that are the mean daily flows of three consecutive days, with the maximum mean daily flow occupying the middle position. A parameter, the value of which lies between zero and two, is designated as base factor K and has a governing influence on the estimated peak. The predicting formula employed assumes that the K value is equal to one"--Abstract, p. v. |
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| 546 | |aIncludes abstract in French. |
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| 692 | 07|2gccst|aStreams |
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| 692 | 07|2gccst|aWater management |
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| 692 | 07|2gccst|aMethodology |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 2 |aNational Hydrology Research Institute (Canada) |
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| 710 | 1 |aCanada. |bInland Waters Directorate. |
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| 830 | #0|aTechnical bulletin (Canada. Inland Waters Directorate)|vno. 122.|w(CaOODSP)9.861123 |
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| 856 | 40|qPDF|s46.09 MB|uhttps://publications.gc.ca/collections/collection_2018/eccc/en36-503/En36-503-122-eng.pdf |
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