approached significanceP = .095
The difference between Short and Long streams for the drift rate approached significance for the Slow streams P = .095; see Fig. 4D , and was not significant in the Fast condition ( P > 0.1; see Fig. 4C ).
The difference between Short and Long streams for the drift rate approached significance for the Slow streams P = .095; see Fig. 4D , and was not significant in the Fast condition ( P > 0.1; see Fig. 4C ).