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001 | 9.864115 |
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003 | CaOODSP |
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005 | 20221107161444 |
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007 | cr ||||||||||| |
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008 | 181102s1986 onca ob f000 0 eng d |
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020 | |z0662543580|q(print) |
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040 | |aCaOODSP|beng |
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041 | |aeng|afre |
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043 | |an-cn--- |
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086 | 1 |aEn36-503/141-PDF|zEn36-503/141 |
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100 | 1 |aSangal, B. P., |d1929- |
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245 | 10|aRecursion formula for unit hydrographs |h[electronic resource] = |bRelation de récurrence pour les hydrogrammes unitaires / |cB.P. Sangal. |
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246 | 31|aRelation de récurrence pour les hydrogrammes unitaires |
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260 | |aOttawa : |bNational Hydrology Research Institute, Inland Waters Directorate = Institut national de recherches en hydrologie, Direction générale des eaux intérieures, |c1986. |
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300 | |av, 14 p. : |bill. |
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490 | 0 |aNHRI paper ; |vno. 29 = |aRapport de l'INRH ; |vn° 29 |
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490 | 1 |aIWD technical bulletin ; |vno. 141 = |aCollection des rapports techniques de la DGEI ; |vétude n° 141 |
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500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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504 | |aIncludes bibliographical references (p. 10). |
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520 | 3 |a"A recursion formula has been derived which can be used for converting unit hydrographs either from short duration to long duration or from long duration to short duration. Thus, an alternative to developing an S-hydrograph for this purpose is proposed. Examples on the use of the formula have been provided. A technique has also been suggested to eliminate oscillations in the S-hydrograph and derived unit hydrograph"--Abstract, p. v. |
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546 | |aText in English and French. |
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693 | 4|aHydrography--Graphic methods |
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693 | 4|aHydrology--Research |
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710 | 1 |aCanada. |bEnvironment Canada. |
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710 | 1 |aCanada. |bInland Waters Directorate. |
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710 | 2 |aNational Hydrology Research Institute (Canada) |
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792 | |tRecursion formula for unit hydrographs |w(CaOODSP)9.864116 |
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830 | #0|aTechnical bulletin (Canada. Inland Waters Directorate)|vno. 141.|w(CaOODSP)9.861123 |
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856 | 40|qPDF|s2.59 MB|uhttps://publications.gc.ca/collections/collection_2018/eccc/en36-503/En36-503-141.pdf |
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