In very shallow water (H &lt; 0.2 d E ) the flow is essentially controlled by wind stress and bottom friction and the Coriolis force becomes insignificant;
(the flow; is essentially controlled; by wind stress and bottom friction and the Coriolis force) (In very shallow water (H &lt; 0.2 d E ) the flow is essentially controlled by wind stress and bottom friction and the Coriolis force; becomes; insignificant)
the flow In very shallow water (H &lt
is essentially controlled 0.2 d E ) the flow is essentially controlled by wind stress and bottom friction and the Coriolis force
by wind stress and bottom friction and the Coriolis force
becomes insignificant