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| 02156nam 2200373za 4500 |
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| 001 | 9.847064 |
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| 003 | CaOODSP |
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| 005 | 20221107153344 |
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| 007 | cr ||||||||||| |
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| 008 | 171114s1985 onca|||fo f000 0 eng d |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn--- |
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| 086 | 1 |aEn13-5/85-10E-PDF |
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| 100 | 1 |aBeltaos, S., |d1944- |
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| 245 | 10|aIce freeze-up and breakup in the lower Thames River |h[electronic resource] : |b1982-83 observations / |cby S. Beltaos. |
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| 260 | |aBurlington, Ont. : |bEnvironmental Hydraulics Section, Hydraulics Division, National Water Research Institute, Canada Centre for Inland Waters, |c1985. |
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| 300 | |aii, 8, [13] p. : |bill. |
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| 490 | 1 |aNWRI contribution ; |v85-10 |
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| 500 | |a"June 1985". |
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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 | 3 |a"The 1982-83 ice season was uneventful due to the unusually mild winter conditions. An ice cover formed in the study reach in mid-January and partly broke up in early February. This breakup produced one ice jam near the Golf Course and was followed by alternating cold and mild weather periods. The remaining thin ice cover deteriorated and disappeared by February 23. Observations concerning breakup initiation and ice jam stage were found to be consistent with previous results which extends the applicability of earlier developed methods to unusually thin ice and low discharge conditions"--Abstract, p. i. |
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| 546 | |aIncludes abstract and management perspective in French. |
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| 692 | 07|2gccst|aRivers |
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| 692 | 07|2gccst|aIce |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 2 |aNational Water Research Institute (Canada) |
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| 794 | |tIce freeze-up and breakup in the lower Thames River |w(CaOODSP)9.847068 |
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| 795 | ##|tIce freeze-up and breakup in the lower Thames River |w9.847059 |
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| 830 | #0|aNWRI contribution ;|vno. 85-10|w(CaOODSP)9.844121 |
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| 856 | 40|qPDF|s1.74 MB|uhttps://publications.gc.ca/collections/collection_2017/eccc/En13-5-85-10-eng.pdf |
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