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040	|aCaOODSP|beng|erda|cCaOODSP
043	|an-cn-bc|an-cn-yk
086	1 |aEn37-529/1988E-PDF
100	1 |aSmith, A. G. |q(Adrian G.)|eauthor.
245	10|aApplication of the logarithmic and stage discharge equation methods for rating curve extension / |cA.G. Smith.
264	1|aVancouver, British Columbia : |bPlanning and Studies Section, Water Resources Branch, |cJuly 1988.
300	|a1 online resource (iv, 41 pages) : |bgraphs
336	|atext|btxt|2rdacontent
337	|acomputer|bc|2rdamedia
338	|aonline resource|bcr|2rdacarrier
500	|aDigitized edition from print [produced by Environment and Climate Change Canada].
504	|aIncludes bibliographical references (page 11).
520	|a"Two methods of rating curve extension - the logarithmic and stage-discharge equation (as developed by Dr. B.P. Sangal) - have been applied to eleven rating curves from ten streams gauging stations in the Pacific and Yukon Region. The data from these stations was readily available from previous studies. The results are comparable, within 10 percent, for six rating curve extensions and of the remaining four the logarithmic method provides a better fit in two. One rating curve was not sufficiently defined for the reliable application of either method. This is not to be considered as a definitive study with so small a sample of rating curves. The recommendation of this study is to apply both methods and then select the one that gives the best results"--Summary, page i.
650	0|aCurves, Logarithmic.
650	0|aStream measurements|zBritish Columbia.
650	0|aStream measurements|zYukon.
650	6|aCourbes logarithmiques.
650	6|aCours d'eau|xJaugeage|zColombie-Britannique.
650	6|aCours d'eau|xJaugeage|zYukon.
710	1 |aCanada. |bWater Resources Branch, |eissuing body.
856	40|qPDF|s3.43 MB|uhttps://publications.gc.ca/collections/collection_2022/eccc/En37-529-1988-eng.pdf