On the variety of internal wave radar observations in the ocean. 1. Slick-like signatures

• Type: Article in International Conference Proceedings Book
• Date: 2000

Authors

Da Silva, JCB (Author) Other; Ermakov, SA (Author) Other; Robinson, IS (Author) Other

Conference proceedings International

Title: European Space Agency, (Special Publication) ESA SP

Pages: 1260-1269

ERS-Envisat Symposium 'Looking Down to Earth in the New Millennium'

Gothenburg, 16 October 2000 through 20 October 2000

Indexing

ISI Web of Knowledge

Scopus - 0 Citations

Other information

Authenticus ID: P-007-BWF

Abstract (EN): It was shown recently that three different types of short-period Internal Wave SAR signatures occur on the Iberian Shelf depending on parameters of surface-active films. Large scale modulation of film characteristics by currents associated with internal tidal waves can also produce a signature in ERS SAR images. On the Western Iberian shelf short-period IWs typically propagate in groups of packets that are believed to be generated by the evolution of internal tidal waves over the shelf. Here it is shown that onshore propagating short-period IWs can exhibit different SAR signatures within the same wave packet according to their position relative to the phase of the internal tidal wave. These transitions of signature mode can be explained by large scale variations of film parameters produced by the internal tidal waves. At low -to- moderate winds leading waves in the IW packets usually exhibit double sign signatures, which evolve to negative sign signatures for the subsequent waves in the packets. At very low, near-threshold, winds the IW signatures can be in the form of the double sign type undergoing transition to positive sign signatures when compared to the background behind the IW packet. This is a consequence of different threshold wind speeds for excitation of Bragg waves at different film pressures. It is demonstrated that there is an increase of unperturbed film pressure in the direction of the ranking order of solitons in a packet of short-period IWs which is predicted by a theoretical model and in agreement with measurements of film elasticity. It is concluded that observations of SAR signature mode transitions are consistent with previous model results, and a diagram describing mode transitions of the IW signatures in relation to film pressure and wind speed is presented. Examples of such transitions in different regions of the global ocean are presented, illustrating where slick-dominated SAR signatures are expected to occur.

Language: English

Type (Professor's evaluation): Scientific