Various, Encyclopaedia Britannica, 11th Edition…
“ If the motion is rectilinear and uniform, the variation of pressure is the same as in a fluid at rest. In a stream flowing in an open channel, for instance, when the effect of eddies produced by the roughness of the sides is neglected, the pressure at each point is simply the hydrostatic pressure due to the depth below the free surface. (b) If the velocity of the fluid is very small, the distribution of pressure is approximately the same as in a fluid at rest. ”
