In order to monitor the temperature variability over the total water c
olumn in a stratified shallow sea, a thermistor string was suspended f
rom a moored loosely tethered surface buoy. Some of the temperature da
ta manifested strong first tidal harmonic variability and unrealistic
thermocline deepening. It is shown that the string lifted under the ac
tion of horizontal buoy displacement. Although the data may be correct
ed by using additional pressure or tilt sensors, a method is given to
detect and correct them using current data, some simple arguments for
buoy displacement under drag force and cross-spectral information from
the first harmonic tidal band. The method proves adequate, as has bee
n verified using temperature data measured at a nearby sub-surface moo
ring and some CTD information. Copyright (C) 1996 Elsevier Science Ltd
.