Numbers along the bottom are station numbers. One contour in each diagram is labelled, and the contour interval is given in the bottom left of each diagram.

The strongly inclined isotherms, isohalines and silicate contours in the deep ocean indicate geostrophic adjustment in the East Australian Current. The patch of low temperature, high salinity and high silicate content on the shelf is the result of an earlier dynamic uplift event. After Middleton et al. (1994)

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