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      <marc:subfield code="a">En57-65/10-77E-PDF</marc:subfield>
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      <marc:subfield code="a">Lo, Aloysius K., </marc:subfield>
      <marc:subfield code="e">author.</marc:subfield>
    </marc:datafield>
    <marc:datafield tag="245" ind1="1" ind2="2">
      <marc:subfield code="a">A critical examination of the significance of the diabatic influence functions and the von Karman constant / </marc:subfield>
      <marc:subfield code="c">by Aloysius K. Lo and Gordon A. McBean.</marc:subfield>
    </marc:datafield>
    <marc:datafield tag="264" ind1=" " ind2="1">
      <marc:subfield code="a">Downsview, Ontario : </marc:subfield>
      <marc:subfield code="b">Boundary Layer Research Division, Air Quality and Inter-Environmental Research Branch, Atmospheric Environment Service, </marc:subfield>
      <marc:subfield code="c">[1977]</marc:subfield>
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      <marc:subfield code="a">computer</marc:subfield>
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      <marc:subfield code="a">Report ARQL ;</marc:subfield>
      <marc:subfield code="v">10/77</marc:subfield>
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    <marc:datafield tag="500" ind1=" " ind2=" ">
      <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 (page 9).</marc:subfield>
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      <marc:subfield code="a">"In studies of flux-profile relationships for wind velocity and temperature, the Monin-Ohukhov similarity theory for the constant flux layer is frequently used. There have been a number of widely accepted forms for the diabatic influence functions proposed in the literature. In many cases different values for the von Karman constant, k, were used to achieve agreement with experimental data. This paper examines the differences in fluxes compiled from the same profile data but using different flux—profile relationships. It is felt that, at least partially, these differences are due to experimental errors and the deviations of the field sites from the ideal conditions that were assumed in the derivation of the Monin-Obukhov Similarity Theory"--Abstract.</marc:subfield>
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      <marc:subfield code="a">Boundary layer (Meteorology)</marc:subfield>
      <marc:subfield code="x">Mathematical models.</marc:subfield>
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      <marc:subfield code="a">Couche limite (Météorologie)</marc:subfield>
      <marc:subfield code="x">Modèles mathématiques.</marc:subfield>
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      <marc:subfield code="a">Canada. </marc:subfield>
      <marc:subfield code="b">Boundary Layer Research Division, </marc:subfield>
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    <marc:datafield tag="710" ind1="1" ind2=" ">
      <marc:subfield code="a">Canada. </marc:subfield>
      <marc:subfield code="b">Air Quality and Inter-Environmental Research Branch, </marc:subfield>
      <marc:subfield code="e">issuing body.</marc:subfield>
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    <marc:datafield tag="710" ind1="1" ind2=" ">
      <marc:subfield code="a">Canada. </marc:subfield>
      <marc:subfield code="b">Atmospheric Environment Service, </marc:subfield>
      <marc:subfield code="e">issuing body.</marc:subfield>
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      <marc:subfield code="a">Report ARQL ;</marc:subfield>
      <marc:subfield code="v">10/77.</marc:subfield>
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      <marc:subfield code="q">PDF</marc:subfield>
      <marc:subfield code="s">550 KB</marc:subfield>
      <marc:subfield code="u">https://publications.gc.ca/collections/collection_2024/eccc/en57/En57-65-10-77-eng.pdf</marc:subfield>
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