| Автор | Csanady, G. T. |
| Автор | Scott, J. T. |
| Дата выпуска | 1980 |
| dc.description | Arithmetic averages of daily temperature and current surveys during July‐August 1972 are used to define a mean summer coastal circulation pattern in Lake Ontario. Some of the important features of this mean flow pattern may be explained by simple equilibrium models of wind‐driven flow. Discrepancies between these models and coastal zone observations appear to be due mainly to advection of momentum during transient flow episodes, especially those involving the intermittent appearance of full upwelling along the north shore. The south shore flow pattern consists of divergent coastal jets, much as the theoretical steady response of a frictionless two‐layer basin to an eastward wind. At the eastern end of the lake a deep current is generated by interface friction below the strong coastal jets. Along the north shore there is no mean coastal jet pattern, and the return flow of warm water must be supposed to be accomplished some distance offshore. |
| Формат | application.pdf |
| Копирайт | Copyright 1980 by the American Geophysical Union. |
| Тема | BIOGEOSCIENCES |
| Тема | Limnology |
| Тема | HYDROLOGY |
| Тема | Limnology |
| Тема | OCEANOGRAPHY: GENERAL |
| Тема | Oceanography: Boundary layer and exchange processes |
| Тема | Oceanography: Circulation |
| Тема | Limnology |
| Тема | PALEOCEANOGRAPHY |
| Тема | Limnology |
| Название | Mean summer circulation in Lake Ontario within the coastal zone |
| Тип | article |
| DOI | 10.1029/JC085iC05p02797 |
| Electronic ISSN | 2156-2202 |
| Print ISSN | 0148-0227 |
| Журнал | Journal of Geophysical Research: Oceans |
| Том | 85 |
| Первая страница | 2797 |
| Последняя страница | 2812 |
| Выпуск | C5 |
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