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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...
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| Format: | Article |
| Language: | Russian |
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Видавничий дім "Академперіодика" НАН України
2007
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| Online Access: | http://dspace.nbuv.gov.ua/handle/123456789/3140 |
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irk-123456789-31402009-07-02T12:00:22Z Транспорт наносов внутренними волнами Слепышев, A.A. Носова, А.В. Науки про Землю 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. 2007 Article Транспорт наносов внутренними волнами / А.А. Слепышев, А.В. Носова // Доп. НАН України. — 2007. — № 9. — С. 95-101. — Бібліогр.: 9 назв. — рос. 1025-6415 http://dspace.nbuv.gov.ua/handle/123456789/3140 551.466.8 ru Видавничий дім "Академперіодика" НАН України |
| institution |
Digital Library of Periodicals of National Academy of Sciences of Ukraine |
| collection |
DSpace DC |
| language |
Russian |
| topic |
Науки про Землю Науки про Землю |
| spellingShingle |
Науки про Землю Науки про Землю Слепышев, A.A. Носова, А.В. Транспорт наносов внутренними волнами |
| description |
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. |
| format |
Article |
| author |
Слепышев, A.A. Носова, А.В. |
| author_facet |
Слепышев, A.A. Носова, А.В. |
| author_sort |
Слепышев, A.A. |
| title |
Транспорт наносов внутренними волнами |
| title_short |
Транспорт наносов внутренними волнами |
| title_full |
Транспорт наносов внутренними волнами |
| title_fullStr |
Транспорт наносов внутренними волнами |
| title_full_unstemmed |
Транспорт наносов внутренними волнами |
| title_sort |
транспорт наносов внутренними волнами |
| publisher |
Видавничий дім "Академперіодика" НАН України |
| publishDate |
2007 |
| topic_facet |
Науки про Землю |
| url |
http://dspace.nbuv.gov.ua/handle/123456789/3140 |
| citation_txt |
Транспорт наносов внутренними волнами / А.А. Слепышев, А.В. Носова // Доп. НАН України. — 2007. — № 9. — С. 95-101. — Бібліогр.: 9 назв. — рос. |
| work_keys_str_mv |
AT slepyševaa transportnanosovvnutrennimivolnami AT nosovaav transportnanosovvnutrennimivolnami |
| first_indexed |
2023-03-24T08:26:45Z |
| last_indexed |
2023-03-24T08:26:45Z |
| _version_ |
1796139046693502976 |