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| 02100cam 2200349zi 4500 |
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| 001 | 9.870888 |
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| 003 | CaOODSP |
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| 005 | 20221107163237 |
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| 006 | m o d f |
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| 007 | cr ||||||||||| |
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| 008 | 190401s1999 onca #ot f000 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |an-cn--- |
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| 086 | 1 |aEn13-5/99-230E-PDF |
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| 100 | 1 |aHe, Cheng, |d1957- |eauthor. |
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| 245 | 10|aAnalytical solutions for testing of 3-D baroclinic and wind driven coastal models / |cby: C. He & P. Hamblin. |
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| 264 | 1|a[Burlington, Ontario] : |bEnvironment Canada, Water Science and Technology Directorate = Environnement Canada, Direction générale des sciences et de la technologie, eau, |c[1999] |
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| 300 | |a1 online resource (19, (6) 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 ; |v99-230 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 504 | |aIncludes bibliographical references. |
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| 520 | |a"It is always challenge for a model developer to verify three dimensional hydrodynamic and transport models, especially for the baroclinic term over variable topography, due to a lack of observational data sets or the availability of suitable analytical solutions. Heat flux through the water surface and wind stress are the two main forces controlling the stratification of a water body. In this paper, exact solutions for periodic forcing by surface heat flux and wind stress, are given by solving the linearized equations of motion in a three dimensional domain neglecting the rotational and horizontal diffusion terms"--Abstract. |
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| 692 | 07|2gccst|aWater management |
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| 700 | 1 |aHamblin, P. F., |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 ;|v99-230.|w(CaOODSP)9.844121 |
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| 856 | 40|qPDF|s1.29 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-99-230-eng.pdf |
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