The Clyde Estuary catchment area received an immense amount of rainfal
l over a short period (9-11 December 1994) with an estimated return pe
riod of over 500 years. The average flow into the Estuary is 156 m(3)
s(-1), and the total peak flow gauged during this event was about 2000
m(3) s(-1). The influx of this water was monitored daily over the fol
lowing week for a single transect across the Largs Channel. A cruise w
as made around the Estuary at the peak of the influx on 16 December. P
rofiles of salinity, temperature and photosynthetically active radiati
on were taken at 38 stations, covering over 34 km. The daily and cruis
e data are presented against background data collected since September
1994 for a single station in the Largs Channel. (C) 1997 Academic Pre
ss Limited.