Ocean temperature climate off north-east New Zealand

The ocean temperature field off the north-east coast of New Zealand is studied to quantify the annual cycle and reveal the intra- and inter-annual variability. The data used are repeat expendable bathythermograph (XBT) sections between Auckland and either Suva or Honolulu which have been collected quarterly since 1986. These sections give temperature measurements between the surface and 800 m and Auckland and 30 degreesS from 1986 to August 1999. The mean and annual cycle are compared with those from the NOAA World Ocean Atlas (WOA98). The results are similar; however WOA98 lacks the horizontal resolution to fully discern the East Auckland Current and North Cape Eddy, while the XBT analysis lacks the temporal resolution to discern higher frequency intra-annual signals. The temperature variability in the mixed layer is dominated by the annual cycle, which accounts for 80-90% of the variance. The amplitude of the annual cycle diminishes rapidly with depth, from 2.8 degreesC at the surface, to c. 0.1 degreesC at 180 m. The phase of the annual cycle is retarded with depth, with peak temperatures occurring in February at the surface and in June/July at 180 m. Removing the annual cycle from the time series reveals the more subtle inter- and intra-annual variability. This variability is of the order of 1 degreesC in the upper 50 m, decreasing to 0.3 degreesC at 400-500 m. The surface layer was cold between 1991 and 1994 (c. 0.7 degreesC cooler than average), and 0.7 degreesC warmer than average in 1999. The deeper ocean shows a different signal, being up to 0.3 degreesC cooler in 1990-92, 0.3 degreesC warmer in 1998, and c. 0.2 degreesC warmer than average in 1999. The inter-annual mixed layer variability is highly correlated with the Southern Oscillation Index and also with inter-annual terrestrial air temperature and wind measurements from northern New Zealand. In contrast, at higher intra-annual frequencies, the mixed layer variability is not correlated with air and wind measurements. At these higher frequencies, the air temperature is better correlated with the sea surface temperature (SST) than with the bulk mixed layer temperature.