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| 02209nam 2200385zi 4500 |
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001 | 9.871672 |
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003 | CaOODSP |
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005 | 20221107163442 |
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006 | m o d f |
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007 | cr ||||||||||| |
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008 | 190416s1998 oncd #ot f000 0 eng d |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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041 | |aeng|bfre |
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043 | |an-cn-bc |
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086 | 1 |aEn13-5/99-207E-PDF |
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100 | 1 |aHamblin, P. F., |eauthor. |
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245 | 10|aBaseline physical limnology of the Upper Arrow Lakes Reservoir / |cby Paul F. Hamblin. |
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264 | 1|a[Burlington, Ontario] : |bNational Water Research Institute, |c1998. |
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300 | |a1 online resource (21, 32 pages) : |bcharts. |
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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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490 | 1 |aNWRI contribution ; |v99-207 |
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500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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500 | |a"December, 1998." |
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504 | |aIncludes bibliographical references. |
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520 | |a"Field observations of temperature and current profiles were taken during August 1997 in the Upper Arrow Lakes Reservoir for the purposes of determining the baseline limnology in the event that lake fertilization would be undertaken to restore the declining Kokanee sports fishery. Highlights and analyses of these observations are provided in this report. Most of the effort was devoted to studying the exchange between the Upper and Lower Lakes and the pattern of flow in the inflow region of the lake. In both cases the circulation was found to be complex and due to the water stratification, bathymetry and the earth’s rotation. Implications are given for the addition of nutrients. At the same time some novel instrumentation were evaluated in this ultra oligotrophic lake"--Abstract. |
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546 | |aIncludes abstract in French. |
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692 | 07|2gccst|aWater management |
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692 | 07|2gccst|aLakes |
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710 | 1 |aCanada. |bEnvironment Canada. |
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710 | 2 |aNational Water Research Institute (Canada) |
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830 | #0|aNWRI contribution ;|v99-207.|w(CaOODSP)9.844121 |
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856 | 40|qPDF|s2.82 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-99-207-eng.pdf |
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