Fig. 6From: Tidal and internal tidal impacts in the Tasman Seaa Time series of the elevation at 30° S 154° 11’E indicating the daily and spring-neap tidal cycles b Difference in flow tangent to the continental shelf break at 200 m between the tidal and non-tidal simulations. c Same as b for water colder than 18 °C. Negative values indicate either an increase in a southward flow or a decrease in a northward flowBack to article page