The physical environment within a California kelp bed is modified from
that of the region by the large drag of the massed plants. The change
is greatest for longshore motions, where velocities diminish with dis
tance upcoast of the leading edge of the bed in a manner consistent wi
th the damping expected for coastally-trapped waves. Cross-shore veloc
ity fluctuations are more important for the movement of material betwe
en offshore waters and the kelp bed interior. Results suggest that pen
etration of water for distances of 400 m into the kelp is common. The
importance of water motions for ecological processes ranging from enha
ncing boundary layer transport to kelp blades to moving planktonic lar
vae implies that size of a kelp bed and position within it are importa
nt for the kelp ecosystem. (C) 1998 Elsevier Science Ltd. All rights r
eserved.