The seasonal variation in the suspended sediment distribution in the S
outhern North Sea has been defined by direct sampling over a grid of s
tations. The East Anglian plume, a region of relatively high concentra
tions, develops eastward from eastern England across the Southern Eigh
t during the winter. During the summer the plume concentrations are lo
wer. Using residual currents obtained from a numerical model, together
with the depth averaged suspended matter concentrations, allows estim
ation of the fluxes within the plume. This suggests that 6.6 x 10(6) t
of suspended matter was transported eastward in one year, with possib
le errors of +/- 50%. Comparison with published sediment budgets for t
he coastal area of eastern England shows that the plume constitutes a
major feature transporting sediment across the North Sea. (C) 1998 Els
evier Science Ltd. All rights reserved.