Current meter data from the coastal ocean at Sydney, south-eastern Australi
a, were analysed to seek evidence of a response to the prevailing summer se
a breeze. A response to the sea breeze was found in the currents. This is s
ignificant since the magnitude of the sea breeze was small by comparison wi
th winds associated with large-scale pressure systems and the East Australi
an Current. Responses were determined by analysing short periods (3-5 days)
of sea breeze activity as opposed to the whole 2-month data set. The corre
lations between the alongshore nearshore diurnal-period currents and the lo
cal wind stress during the sea breeze periods were significantly higher tha
n the correlations during non-sea-breeze periods. Despite the stronger corr
elations the sea breeze could only account for around one-quarter of the Va
riance in the diurnal-period currents. However, the detection of the respon
se to the sea breeze is significant since the sea breeze has never previous
ly been identified as a process for forcing alongshore nearshore currents o
n this shelf.