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040 |aCaOODSP|beng|erda|cCaOODSP
041 |aeng|bfre
043 |an-cn-nf
0861 |aEn13-5/87-140E-PDF
1001 |aNg, H. Y. F., |eauthor.
24510|aStreamflow forecasting with HSPF modelling experience / |cby Howard Ng.
264 1|aBurlington, Ontario : |bNational Water Research Institute, Rivers Research Branch, Canada Centre for Inland Waters, |cSeptember 1987.
300 |a1 online resource (11 pages, 10 unnumbered pages) : |bmaps, graphs.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aNWRI contribution ; |v87-140
500 |a"RRB-87-55."
500 |aTitle from cover.
500 |a"Prepared for presentation at Third Streamflow Forecasting Meeting, Toronto, October 21-22, 1987."
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
504 |aIncludes bibliographical references.
5203 |a"The Hydrologic Simulation Program - Fortran (HSPF) of the U.S. Environmental Protection Agency has been applied for simulation of the hydrological response of an urbanizing watershed. The calibrated HSPF model was then applied to future land use development scenarios. It was noted that an expected increase in the impervious area in the watershed is unlikely to increase the volume of streamflow, but it would contribute to increases in flow peaks and the incidence of flooding. If the impervious area is doubled in the watershed, the flow peaks may increase by 20%"--Abstract.
546 |aIncludes a management perspective and abstract in English and French.
69207|2gccst|aWatersheds
69207|2gccst|aFloods
69207|2gccst|aModels
7101 |aCanada. |bEnvironment Canada.
7102 |aNational Water Research Institute (Canada). |bRivers Research Branch.
7102 |aCanada Centre for Inland Waters.
830#0|aNWRI contribution ;|v87-140.|w(CaOODSP)9.844121
85640|qPDF|s1.39 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-87-140-eng.pdf