Abstract
The transition from the early surface-reflected to near-surface-refracted waves is associated with a triplication pattern of arrivals which is very sensitive to upper ocean processes, including mixed layer formation, spicy fronts and internal waves. The pattern is well sampled at surface-conjugate depths (3 to 5 km). Deep and relatively short vertical arrays operating in the still, uniform abyssal environment are an attractive alternative to shallow in situ measurements.
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