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      <marc:subfield code="a">En13-5/93-17E-PDF</marc:subfield>
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      <marc:subfield code="a">Rogers, Christopher K., </marc:subfield>
      <marc:subfield code="e">author.</marc:subfield>
    </marc:datafield>
    <marc:datafield tag="245" ind1="1" ind2="0">
      <marc:subfield code="a">Observations and numerical simulation of a small ice-covered mid-latitude lake / </marc:subfield>
      <marc:subfield code="c">by Christopher K. Rogers, Paul F. Hamblin, Gregory A. Lawrence.</marc:subfield>
    </marc:datafield>
    <marc:datafield tag="264" ind1=" " ind2="1">
      <marc:subfield code="a">Burlington, Ontario : </marc:subfield>
      <marc:subfield code="b">Lakes Research Branch, National Water Research Institute, </marc:subfield>
      <marc:subfield code="c">March 2, 1993.</marc:subfield>
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      <marc:subfield code="a">1 online resource (28, [4] pages) : </marc:subfield>
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      <marc:subfield code="b">txt</marc:subfield>
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      <marc:subfield code="a">computer</marc:subfield>
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      <marc:subfield code="2">rdamedia</marc:subfield>
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      <marc:subfield code="a">online resource</marc:subfield>
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      <marc:subfield code="a">NWRI contribution ; </marc:subfield>
      <marc:subfield code="v">93-17</marc:subfield>
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      <marc:subfield code="a">Digitized edition from print [produced by Environment and Climate Change Canada].</marc:subfield>
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    <marc:datafield tag="504" ind1=" " ind2=" ">
      <marc:subfield code="a">Includes bibliographical references (pages 25-27).</marc:subfield>
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    <marc:datafield tag="520" ind1=" " ind2=" ">
      <marc:subfield code="a">"An existing heat transfer algorithm is extended to permit the simulation of ice and snow cover on a small mid-latitude lake. New features include: snowmelt due to rain, sediment heat transfer, snow-ice formation, and variability in snow density, snow conductivity and albedo. Since the lake considered is nearly isothermal in winter, the new model ignores internal thermodynamics. All discrepancies between field observations and model predictions are accounted for by parameter uncertainties and expected observation error. It was found that sediment heat transfer may be irnportant in early winter in preventing a net loss of heat from the lake water. Significant heat gains in the latter part of winter, however, are attributed to the penetration of solar radiation through the ice"--Abstract.</marc:subfield>
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      <marc:subfield code="2">gccst</marc:subfield>
      <marc:subfield code="a">Lakes</marc:subfield>
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      <marc:subfield code="a">Hamblin, P. F., </marc:subfield>
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      <marc:subfield code="a">Lawrence, Gregory A‏., </marc:subfield>
      <marc:subfield code="e">author.</marc:subfield>
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      <marc:subfield code="a">Canada. </marc:subfield>
      <marc:subfield code="b">Environment Canada.</marc:subfield>
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      <marc:subfield code="a">National Water Research Institute (Canada). </marc:subfield>
      <marc:subfield code="b">Lakes Research Branch.</marc:subfield>
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      <marc:subfield code="a">NWRI contribution ;</marc:subfield>
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      <marc:subfield code="w">(CaOODSP)9.844121</marc:subfield>
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      <marc:subfield code="q">PDF</marc:subfield>
      <marc:subfield code="s">2.65 MB</marc:subfield>
      <marc:subfield code="u">https://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-93-17-eng.pdf</marc:subfield>
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