Sutton & Roemmich--Ocean temperature climate

New Zealand Journal of Marine and Freshwater Research abstracts

Ocean temperature climate off north-east New Zealand

PHILIP J. H. SUTTON

National Institute of Water & Atmospheric
Research Ltd
P. O. Box 14 901, Kilbirnie
Wellington, New Zealand
email: p.sutton@niwa.cri.nz

DEAN ROEMMICH

Scripps Institution of Oceanography
University of California, San Diego
La Jolla, CA 92093
United States

Abstract 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°S 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°C at the surface, to c. 0.1°C 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°C in the upper 50 m, decreasing to 0.3°C at 400-500 m. The surface layer was cold between 1991 and 1994 (c. 0.7°C cooler than average), and 0.7°C warmer than average in 1999. The deeper ocean shows a different signal, being up to 0.3°C cooler in 1990-92, 0.3°C warmer in 1998, and c. 0.2°C 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.

Keywords East Auckland Current; ocean temperature variability; North Cape Eddy; Southern Oscillation Index

New Zealand Journal of Marine and Freshwater Research, 2001, Vol. 35: 553-565

0028-8330/01/3503-0553 $7.00 (c) The Royal Society of New Zealand 2001

PDF file of entire paper: medium quality (2520K); (scanned from paper original: notes about this process)

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