Sm. Chiswell, VARIABILITY IN SEA-SURFACE TEMPERATURE AROUND NEW-ZEALAND FROM AVHRR IMAGES, New Zealand Journal of Marine and Freshwater Research, 28(2), 1994, pp. 179-192
Multi-channel Advanced Very-High Resolution Radiometer (AVHRR) images
of sea surface temperature (SST) in the New Zealand region have been a
rchived since 1989. The first 2 years of data are used to investigate
the variability in sea surface temperature (SST) and its gradients aro
und New Zealand. Empirical orthogonal function (EOF) analyses show tha
t the annual cycle accounts for 92% of the variance of SST, but for le
ss of the variance in SST gradient. The Southland and Subantarctic Fro
nts have an annual modulation in their strengths, accounting for about
20% of their variance; these modulations are out of phase, with the S
outhland Front being strongest in winter. The Subtropical Convergence
shows variability that cannot be easily described by one mode, but app
ears to migrate meridionally with an annual period, being furthest nor
th in March.