| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.868603 |
| 003 | CaOODSP |
| 005 | 20241203113646 |
| 006 | m o d f |
| 007 | cr ||||||||||| |
| 008 | 190220s2004 onc #ot f|0| 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 041 | |aeng|bfre |
| 043 | |an-cn-on |
| 086 | 1 |aEn13-5/04-176E-PDF |
| 100 | 1 |aSheng, Jinyu, |d1959- |eauthor. |
| 245 | 10|aDevelopment of a three-dimensional hydrodynamic circulation model for Lake Huron and Georgian Bay / |cJinyu Sheng and Yerubandi R. Rao. |
| 264 | 1|aBurlington, Ontario : |bNational Water Research Institute, Environment Canada, |c[2004] |
| 300 | |a1 online resource (16 pages): |bfigures. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aNWRI contribution ; |v04-176 |
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
| 504 | |aIncludes bibliographic references. |
| 520 | |a"A primitive equation z-level ocean circulation model known as CANDIE (Canadian Version of Diecast, Sheng et al., 1998) is used in the development of a three-dimensional circulation model for Lake Huron and Georgian Bay. The lake circulation model domain covers the region between 275.3°E (84.7°E) and 280.6°E (79.4°W) and between 43°N and 46.3°N, with a horizontal resolution of roughly 2.5 km and 30 z-levels in the vertical. The model is used to simulate the large-scale circulation, temperature distribution and their seasonal variability in 1974-75, during which a field program was conducted in Lake Huron"--Abstract. |
| 546 | |aIncludes abstract in French. |
| 692 | 07|2gccst|aLakes |
| 692 | 07|2gccst|aWater management |
| 700 | 1 |aRao, Yerubandi R., |eauthor. |
| 710 | 1 |aCanada. |bEnvironment Canada. |
| 710 | 2 |aNational Water Research Institute (Canada) |
| 830 | #0|aNWRI contribution ;|v04-176. |w(CaOODSP)9.844121 |
| 856 | 40|qPDF|s1.45 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en13-5/En13-5-04-176-eng.pdf |