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| 02117nam 2200397zi 4500 |
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| 001 | 9.882456 |
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| 003 | CaOODSP |
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| 005 | 20221107170312 |
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| 006 | m o d f |
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| 007 | cr |n||||||||| |
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| 008 | 191126e197512##onc 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 |aEn36-522/55-1975E-PDF |
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| 100 | 1 |aSkafel, M. G., |eauthor. |
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| 245 | 10|aComputation of wave refraction and longshore sediment transport rates / |cby M.G. Skafel. |
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| 264 | 1|a[Burlington, Ontario] :|bCanada Centre for Inland Waters, |cDecember 1975. |
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| 300 | |a1 online resource (56 unnumbered pages) |
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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 |aUnpublished report |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 504 | |aIncludes bibliographical references page [16]. |
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| 520 | 3 |a"A computer programme to calculate wave refraction, wave height and resulting longshore sediment transport is described. Linear theory is used to describe the waves up to the breaker zone. The longshore sediment transport rate is then evaluated using the wave characteristics at breaking. The waves need not originate in deep water, a useful feature when the offshore wave data are hindcasted for shallow lakes. The computed wave direction and height for a plane sloping bathymetry compare favourably to analytical results and to the results of another programme (Dobson, 1967)"--Abstract. |
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| 546 | |aIncludes abstract in French. |
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| 650 | 0|aWater waves|xComputer simulation. |
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| 650 | 0|aSediment transport. |
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| 650 | 6|aVagues|xSimulation par ordinateur. |
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| 650 | 6|aSédiments (Géologie)|xTransport. |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 2 |aCanada Centre for Inland Waters. |
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| 830 | #0|aUnpublished report (Canada Centre for Inland Waters)|w(CaOODSP)9.881827 |
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| 856 | 40|qPDF|s2.03 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en36-522/En36-522-55-1975-eng.pdf |
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