ملخص
The importance of an existing criterion, to distinguish between ordinary and quasi-steady wave boundary layers, has been elucidated by considering two typical field examples. It has been shown that only longer period of oscillation is not sufficient to induce quasi-steady properties, the ratio of boundary layer thickness to the distance from the bottom to free-stream must be used instead, in order to distinguish a quasi-steady wave boundary layer from an ordinary one.
اللغة الأصلية | English |
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الصفحات | 233-242 |
عدد الصفحات | 10 |
حالة النشر | Published - 1997 |
منشور خارجيًا | نعم |
الحدث | Proceedings of the 1997 3rd International Conference on Computer Modelling of Seas and Coastal Regions, COASTAL'97 - La Coruna, Spain المدة: يونيو ١ ١٩٩٧ → يونيو ١ ١٩٩٧ |
Other
Other | Proceedings of the 1997 3rd International Conference on Computer Modelling of Seas and Coastal Regions, COASTAL'97 |
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المدينة | La Coruna, Spain |
المدة | ٦/١/٩٧ → ٦/١/٩٧ |
ASJC Scopus subject areas
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