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001 | 9.898843 |
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003 | CaOODSP |
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005 | 20221107174946 |
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006 | m o d f |
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007 | cr bn||||||||| |
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008 | 210407e198003##qucbdo ob f000 0 eng d |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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043 | |an-cn-yk|an-cn-nt|an-cn-bc |
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086 | 1 |aEn37-448/1980E-PDF |
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100 | 1 |aGrey, B. J., |eauthor. |
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245 | 10|aLiard River Basin spring flood : |bprogress report / |cB.J. Grey, D.A. Sherstone ; prepared by Snow & Ice Division, N.H.R.I., Inland Waters Directorate, Environmental Management Service, Environment Canada. |
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264 | 1|aHull, Quebec : |bDepartment of Indian Affairs and Northern Development, Northern Program, Water Resources Program Headquarters, |cMarch 1980. |
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300 | |a1 online resource (1 volume (various pagings)) : |bmaps, graphs, photographs |
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336 | |atext|btxt|2rdacontent |
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337 | |acomputer|bc|2rdamedia |
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338 | |aonline resource|bcr|2rdacarrier |
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500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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504 | |aIncludes bibliographical references (page 87). |
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520 | |a"Aerial reconnaissance and ground monitoring were used to determine the characteristics, pattern and timing of river ice break-up on the Liard River. Ice jams and their associated effects were studied, and channel morphometry was investigated at two ice jam-prone sites. A limited program to measure pre-break-up ice thickness was initiated. Ice thickness was variable across the channel, and decreased rapidly immediately before break-up. Discharge increase was the major factor in initiating and sustaining break-up"--Synopsis. |
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650 | 0|aFlood control|zLiard River. |
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650 | 0|aIce on rivers, lakes, etc.|zLiard River. |
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650 | 6|aInondations|xMaîtrise|zLiard, Rivière au. |
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650 | 6|aGlace sur les cours d'eau, lacs, etc.|zLiard, Rivière au. |
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710 | 1 |aCanada. |bEnvironment Canada. |bInland Waters Directorate, |eissuing body. |
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710 | 1 |aCanada. |bDepartment of Indian Affairs and Northern Development, |eissuing body. |
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856 | 40|qPDF|s38.38 MB|uhttps://publications.gc.ca/collections/collection_2021/eccc/en37/En37-448-1980-eng.pdf |
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