Abstract

A model study using coherent ray-tracing methods was based on a cold-water eddy measured in the Altantic. The eddy, whose diameter is about 320 km was passed through the propagation path at a rate of 4 km/day between a fixed source and fixed receiver separated 445 km. A brief description of the range-dependent model required for this study is presented. The major effects of the eddy were in changing the ray type (number of cycles, RR–RSR, etc.) and in the travel time which had a major effect on the multipath resultant. Time series of amplitude and phase are presented with a qualitative comparison to previously measured data.

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