Транспорт наносов внутренними волнами
In the Boussinesq approximation, the mean flows induced by a wave through nonlinearities in the presence of eddy viscosity are determined for internal waves. The boundary layer solutions, decrement of fading of a wave, and tangential stress at the bottom are determined. The bottom concentration of w...
Збережено в:
| Дата: | 2007 |
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| Автори: | , |
| Формат: | Стаття |
| Мова: | Russian |
| Опубліковано: |
Видавничий дім "Академперіодика" НАН України
2007
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| Теми: | |
| Онлайн доступ: | http://dspace.nbuv.gov.ua/handle/123456789/3140 |
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| Назва журналу: | Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| Цитувати: | Транспорт наносов внутренними волнами / А.А. Слепышев, А.В. Носова // Доп. НАН України. — 2007. — № 9. — С. 95-101. — Бібліогр.: 9 назв. — рос. |
Репозитарії
Digital Library of Periodicals of National Academy of Sciences of Ukraine| Резюме: | In the Boussinesq approximation, the mean flows induced by a wave through nonlinearities in the presence of eddy viscosity are determined for internal waves. The boundary layer solutions, decrement of fading of a wave, and tangential stress at the bottom are determined. The bottom concentration of wave-suspended sediments is obtained when the bottom stress exceeds a critical value. The vertical distribution of the concentration of sediments is determined in the diffusion approximation. |
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