Fig. 8
a Time series of the elevation at 30° S 154° 11’E indicating the daily and spring-neap tidal cycles. b Difference in flow normal to the continental shelf/slope 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 westward flow or a decrease in an eastward flow