The behaviour of the shear velocity along a gravel-bed channel is investiga
ted experimentally in the presence of a negative pressure gradient (acceler
ating flow). Different methods of estimation of the sheer velocity, derived
from vertical profiles of the mean longitudinal point velocity, are examin
ed and a new method is proposed. Results show that the proposed method of e
stimation is comparable to the St Venant and Clauser's methods. At a specif
ic cross section, for constant bottom slope and relative roughness, shear v
elocity increases with discharge.