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001 | 9.904291 |
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003 | CaOODSP |
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005 | 20221107180514 |
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006 | m o d f |
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007 | cr |n||||||||| |
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008 | 211018e198408##oncd ob f000 0 eng d |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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041 | |aeng|beng|bfre |
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086 | 1 |aEn36-539/38-1984E-PDF |
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100 | 1 |aDonelan, M. A. |q(Mark A.), |d1942- |eauthor. |
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245 | 10|aComparison of bulk and direct methods for estimating fluxes and structure function constants over water / |cby M.A. Donelan, R. Golus and H.A. Panofsky. |
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264 | 1|aBurlington, Ontario : |bEnvironment Canada, National Water Research Institute = Environnement Canada, Institut national de recherche sur les eaux, |cAugust 1984. |
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300 | |a1 online resource (iv, 33 pages, 9 unnumbered pages) : |bcharts. |
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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490 | 1 |a[Unpublished manuscript] |
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500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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500 | |a"This manuscript has been submitted to the Journal of Boundary Layer Meteorology for publication and the contents are subject to change." |
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504 | |aIncludes bibliographical references (pages 29 to 32). |
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520 | 3 |a"A set of observations of wind, temperature and moisture over Lake Ontario, under largely stable conditions, has been used to obtain flux—gradient relationships and to test bulk methods for computing stress, heat flux, evaporation and structure function constants. Although the stress-velocity gradient relationship agreed with that observed over land, the heat flux-temperature gradient was quite different"--Abstract. |
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546 | |aIncludes abstracts in French. |
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650 | 0|aAtmospheric thermodynamics. |
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650 | 6|aThermodynamique de l'atmosphère. |
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710 | 2 |aNational Water Research Institute (Canada), |eissuing body. |
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830 | #0|aUnpublished manuscript (National Water Research Institute (Canada))|w(CaOODSP)9.901451 |
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856 | 40|qPDF|s1.88 MB|uhttps://publications.gc.ca/collections/collection_2021/eccc/en36-539/En36-539-38-1984-eng.pdf |
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