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| 02008cam 2200373za 4500 |
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| 001 | 9.848893 |
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| 003 | CaOODSP |
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| 005 | 20221107153803 |
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| 007 | cr ||||||||||| |
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| 008 | 171215s1985 onca|||fob|||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 |aEn13-5/85-154E-PDF |
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| 100 | 1 |aSimons, T. J. |q(Theodore Johannes), |d1939-1987. |
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| 245 | 14|aThe mean circulation of unstratified water bodies |h[electronic resource] / |cby T.J. Simons. |
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| 260 | |aBurlington, Ont. . : |bAquatic Physics and Systems Division, National Water Research Institute, Canada Centre for Inland Waters, |c1985. |
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| 300 | |a12, [4] p. : |bill. |
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| 490 | 1 |aNWRI contribution ; |v85-154 |
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| 500 | |a"August 1985". |
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| 500 | |a"Control No. AP216". |
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| 500 | |a"This manuscript has been submitted to the Journal of Physical Oceanography for publication and the contents are subject to change". |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 504 | |aIncludes bibliographical references: p. 11-12. |
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| 520 | 3 |a"A critical evaluation is presented of the conventional view that long-term mean circulations of homogeneous basins may be identified with the quasi-steady response of linear models to atmospheric forcing. Based on climatological wind records for the Great Lakes region, it is shown that the mean circulation for unstratified seasons is dominated by rectified effects of nonlinear topographic wave interactions"--Abstract. |
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| 546 | |aIncludes executive summary and abstract in English and French. |
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| 692 | 07|2gccst|aLakes |
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| 700 | 1 |aSchertzer, William M. |
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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 ;|vno. 85-154|w(CaOODSP)9.844121 |
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| 856 | 40|qPDF|s1.13 MB|uhttps://publications.gc.ca/collections/collection_2017/eccc/En13-5-85-154-eng.pdf |
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