North Atlantic and equatorial Atlantic Oceans are examined. In general, the PDFs are
approximately Gaussian for small velocities, but with significant exponential tails for large
velocities. Correspondingly, the kurtoses of the distributions are greater than three. Similar
PDFs are found in both western and eastern regions, above and below 1000-m depth, with
more significant non-Gaussianity in the North Atlantic than at the equator. Analogously …