000 02226nam  2200361za 4500
0019.847068
003CaOODSP
00520221107153344
007cr |||||||||||
008171114s1987    onca|||fo    f000 0 eng d
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn---
0861 |aEn13-5/87-19E-PDF
1001 |aBeltaos, S., |d1944-
24510|aIce freeze-up and breakup in the lower Thames River |h[electronic resource] : |b1983-84 observations / |cby S. Beltaos.
260 |aBurlington, Ont. : |bEnvironmental Hydraulics Section, Hydraulics Division, National Water Research Institute, Canada Centre for Inland Waters, |c1985.
300 |aii, 18, [42] p. : |bill.
4901 |aNWRI contribution ; |v87-19
500 |a"February 1987".
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
504 |aIncludes bibliographical references.
5200 |a"This is the fifth report from a continuing program of annual monitoring of ice processes aimed at developing solutions related to ice-jam flooding during breakup. The data presented in this report support methods developed at NWRI to predict the onset of breakup and the release of ice jams in the upper portion of the study reach. The breakup process is more complex in the lower portion of the study reach due to the strong influence of Lake St. Clair on the water levels. Formulation of analogous predictive methods for this reach requires development of new knowledge on the interaction between an ice jam and the intact ice cover downstream. Ice jam stages measured throughout the study reach support the use of an existing theory"--Management perspective.
546 |aIncludes abstract and management perspective in French.
69207|2gccst|aRivers
69207|2gccst|aIce
7101 |aCanada. |bEnvironment Canada.
7102 |aNational Water Research Institute (Canada)
795##|tIce freeze-up and breakup in the lower Thames River |w9.847064
830#0|aNWRI contribution ;|vno. 87-19|w(CaOODSP)9.844121
85640|qPDF|s5.09 MB|uhttps://publications.gc.ca/collections/collection_2017/eccc/En13-5-87-19-eng.pdf