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| 02127cam 2200385zi 4500 |
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| 001 | 9.877912 |
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| 003 | CaOODSP |
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| 005 | 20221107165110 |
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| 006 | m go d f |
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| 007 | cr |n||||||||| |
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| 008 | 190813s199003##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 |aEn13-5/90-117E-PDF |
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| 100 | 1 |aDoering, John Robert Caley, |eauthor. |
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| 245 | 10|aWave height prediction using TMA / |cby J.C. Doering and C.T. Bishop. |
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| 264 | 1|a[Burlington, Ontario] : |bResearch and Applications Branch, National Water Research Institute, |cMarch 1990. |
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| 300 | |a1 online resource (1 volume (various pagings)) : |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 ; |v90-117 |
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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 [17-18]). |
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| 520 | |a"A comparison of the TMA and linear theory methods of wave height prediction is presented. Data from the shoaling waves experiment conducted in Lake Ontario during the fall of 1987 and from laboratory experiments designed to complement the field data are used. The analysis of the laboratory data demonstrates that wave height is predicted slightly more accurately by the TMA method than by a simple linear wave model but with a bias to underpredict. Although the analysis of the field data is not as strongly conclusive as the laboratory data, the same result is obtained"--Abstract. |
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| 546 | |aIncludes abstract in French. |
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| 692 | 07|2gccst|aHydrography |
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| 692 | 07|2gccst|aLakes |
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| 700 | 1 |aBishop, Craig Timothy, |d1953- |eauthor. |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 2 |aNational Water Research Institute (Canada). |bResearch and Applications Branch. |
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| 830 | #0|aNWRI contribution ;|v90-117. |w(CaOODSP)9.844121 |
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| 856 | 40|qPDF|s1.52 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-90-117-eng.pdf |
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