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| 01902cam 2200373zi 4500 |
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| 001 | 9.877873 |
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| 003 | CaOODSP |
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| 005 | 20221107165104 |
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| 006 | m go d f |
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| 007 | cr |n||||||||| |
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| 008 | 190813s1991 oncd #otb 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 |aEn13-5/91-124E-PDF |
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| 100 | 1 |aDonelan, M. A. |q(Mark A.), |d1942- |eauthor. |
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| 245 | 14|aThe mechanical coupling between air and sea : |ban evolution of ideas and observations / |cMark 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 (13, [8] pages) : |bfigures. |
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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 ; |v91-124 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 500 | |aCover title. |
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| 504 | |aIncludes bibliographical references (pages 11-12). |
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| 520 | |a"The roughness of a water surface is parametrized in terms of the wind speed and wave age. Although the variation of equivalent drag coefficient over typical wave age ranges is not large, the distribution of momentum input to the spectrum moves towards the peak in young seas. The implications of this and the inevitable high wind speed saturation of short waves are discussed in the context of scatterometry"--Abstract. |
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| 546 | |aIncludes abstract in French. |
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| 692 | 07|2gccst|aHydrography |
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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 ;|v91-124. |w(CaOODSP)9.844121 |
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| 856 | 40|qPDF|s1.97 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-91-124-eng.pdf |
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