Propagation speeds of strongly nonlinear near-surface internal waves in the Strait of Georgia

A novel aerial observational method for studying internal features in the coastal ocean is developed and tested in a study of large nonlinear internal solitary‐like waves. Photogrammetrically rectified oblique photo images from a circling aircraft are used to track a number of internal wave packets...

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Bibliographic Details
Published inJournal of Geophysical Research Vol. 116; no. C10
Main Authors Wang, C., Pawlowicz, R.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.10.2011
American Geophysical Union
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Summary:A novel aerial observational method for studying internal features in the coastal ocean is developed and tested in a study of large nonlinear internal solitary‐like waves. Photogrammetrically rectified oblique photo images from a circling aircraft are used to track a number of internal wave packets for periods of up to one hour in the Strait of Georgia, British Columbia, Canada. Combining these sequences with coincident water column data allows us to obtain a more complete view of the spatial structure of internal waves. Highly accurate measurements of wave propagation speeds and directions are possible. The applicability of various weakly nonlinear theories in modeling propagation of the observed large‐amplitude waves is tested. The measured wave speeds enable us to differentiate between classic internal wave models. The linear, KdV (Korteweg‐de Vries), and BO (Benjamin‐Ono) models are applied with and without background shear. After background shear effects are included, it is found that a continuously stratified BO equation can predict propagation speeds within observational error, and that this is not true for other theories. The technique may be useful in future studies of oblique internal wave interactions. Key Points Developed a method for studying internal features in the coastal ocean Precise measurements of phase speed can characterize internal waves Benjamin‐Ono equation has been shown useful for large‐amplitude internal waves
Bibliography:ark:/67375/WNG-TJN0JT2B-M
ArticleID:2010JC006776
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SourceType-Scholarly Journals-1
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content type line 23
ISSN:0148-0227
2169-9275
2156-2202
2169-9291
DOI:10.1029/2010JC006776