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| 02159cam 2200361zi 4500 |
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001 | 9.877111 |
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003 | CaOODSP |
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005 | 20221107164903 |
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006 | m o d f |
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007 | cr bn||||||||| |
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008 | 190729s1994 onca ob f000 0 eng d |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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041 | 0 |aeng|beng|bfre |
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043 | |an-cn-on |
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086 | 1 |aEn13-5/94-57E-PDF |
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100 | 1 |aTerray, Eugene A., |eauthor. |
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245 | 10|aEstimates of kinetic energy dissipation under breaking waves / |cby E.A. Terray [and seven others]. |
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264 | 1|aBurlington, Ontario : |bNational Water Research Institute = Institut national de recherche sur les eaux, |c1994. |
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300 | |a1 online resource (1 volume (various pagings)) : |billustrations. |
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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 ; |vno. 94-57 |
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500 | |a"Revision dated 5 April 1994." |
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500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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504 | |aIncludes bibliographical references (pages 26-30). |
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520 | |a"The mixing of surface waters by wave action bears directly on many practical problems and phenomena associated with the use of lakes as a resource; e.g. the dispersal of buoyant pollutants (sewage, oil spills); gas transfer across the air-water interface; nutrient mixing; photosynthetic efficiency of plankton. This study reveals new information on the structure of the turbulence in the upper layers beneath breaking waves. It is shown that the dissipation rates of kinetic energy are many times larger than the traditional estimates. A structure for the near surface layers is described and may be used for modelling in lakes and oceans"--Management perspective. |
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546 | |aIncludes summaries and abstracts in English and French. |
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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. 94-57.|w(CaOODSP)9.844121 |
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856 | 40|qPDF|s4.13 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-94-57-eng.pdf |
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