On the generation of lateral internal waves by a surface seiche in a partially mixed estuary

Dyer (1982) observed internal oscillations in Southampton Water of predominantly 8 and 4 min periods. These were thought to be lateral standing waves generated by the interaction of the first- and second-order surface seiches, respectively, with estuarine topography. The present paper extends the wo...

Full description

Saved in:
Bibliographic Details
Published inEstuarine, coastal and shelf science Vol. 24; no. 4; pp. 557 - 566
Main Authors New, A.L., Dyer, K.R.
Format Journal Article
LanguageEnglish
Published London Elsevier Ltd 1987
Elsevier
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Dyer (1982) observed internal oscillations in Southampton Water of predominantly 8 and 4 min periods. These were thought to be lateral standing waves generated by the interaction of the first- and second-order surface seiches, respectively, with estuarine topography. The present paper extends the work of Rattray (1960) to model the cross-sectional topography of Southampton Water, and shows that internal waves of the observed periods, wavelengths and amplitudes could indeed have been generated in the manner envisaged, but only near the times of certain internal resonant conditions. In general, about two or three such resonances occur per half tidal cycle, and this is in qualitative agreement with Dyer's observations.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0272-7714
1096-0015
DOI:10.1016/0272-7714(87)90134-X