On linear stability of shear flows of an ideal stratified fluid: research methods and new results Научная публикация
Журнал |
Journal of Physics: Conference Series
ISSN: 1742-6588 |
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Вых. Данные | Год: 2019, Том: 1392, Номер: 1, Номер статьи : 012006, Страниц : 6 DOI: 10.1088/1742-6596/1392/1/012006 | ||||||
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Организации |
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Реферат:
The results, that obtained by the spectral method with use of integral relations for the problem of linear stability of steady-state shear plane-parallel flows of an inviscid stratified incompressible fluid in the gravity field with respect to plane perturbations in the Boussinesq approximation and without it, are specied, complemented and developed by the most powerful analytical method of the modern mathematical theory of hydrodynamic stability - the second (or direct) Lyapunov method. In both case, the new analytical method made it possible to prove that given steady-state
flows of stratified fluid are absolutely unstable in theoretical sense with respect to small plane perturbations and to obtain the sufficient conditions for practical linear instability of considered flows. The illustrative analytical examples of given steady-state flows and small plane perturbations as normal waves imposed on them are constructed. Using
the asymptotic method, it is proved that constructed perturbations grow in time irrespective of the fact whether the Miles-Howard and the Miles-type theorems are valid or not.
Библиографическая ссылка:
Gavrilieva A.A.
, Gubarev Y.G.
On linear stability of shear flows of an ideal stratified fluid: research methods and new results
Journal of Physics: Conference Series. 2019. V.1392. N1. 012006 :1-6. DOI: 10.1088/1742-6596/1392/1/012006 Scopus РИНЦ OpenAlex
On linear stability of shear flows of an ideal stratified fluid: research methods and new results
Journal of Physics: Conference Series. 2019. V.1392. N1. 012006 :1-6. DOI: 10.1088/1742-6596/1392/1/012006 Scopus РИНЦ OpenAlex
Идентификаторы БД:
Scopus: | 2-s2.0-85078193667 |
РИНЦ: | 43229246 |
OpenAlex: | W3195465533 |
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