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| 02233cam 2200385zi 4500 |
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001 | 9.877714 |
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003 | CaOODSP |
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005 | 20221107165040 |
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006 | m o d f |
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007 | cr ||||||||||| |
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008 | 190809s1991 onca ob 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--- |
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086 | 1 |aEn13-5/91-114E-PDF |
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100 | 1 |aOcampo-Torres, F. J., |eauthor. |
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245 | 10|aDrift velocity profiles as inferred from measurements of surface wave celerity / |cF.J. Ocampo-Torres and M.A. Donelan. |
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264 | 1|aBurlington, Ontario : |bNational Water Research Institute = Institut national de recherche sur les eaux, |c[1991] |
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300 | |a1 online resource (19 pages, 8 unnumbered pages) : |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 ; |v91-114 |
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500 | |aTitle from cover. |
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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 14-17). |
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520 | |a"The properties of the very thin layer (a few centimeters thick) at the top of a water body determines the mass transfer rate for most toxic anthropogenic gases. Consequently, a great deal of effort is put into measuring and understanding the mechanical properties of this layer. This paper describes a new method of estimating the velocity profile in this layer. The method uses the measured propagation speed of surface waves as a tracer of the velocity profile. It has the considerable merit that the measurements, like the waves, are referenced to the moving surface rather than a-fixed probe"--Management perspective. |
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546 | |aIncludes abstract and management perspective in English and French. |
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692 | 07|2gccst|aWater management |
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700 | 1 |aDonelan, M. A. |q(Mark A.), |d1942- |eauthor. |
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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 ;|v91-114.|w(CaOODSP)9.844121 |
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856 | 40|qPDF|s1.81 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-91-114-eng.pdf |
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