The measurement of the deviation of the 2 -3 leptonic mixing from maximal, D 23 1=2 ÿ sin 2 23 , is one of the key issues for understanding the origin of the neutrino masses and mixing. In the 3 context we study the dependence of various observables in the atmospheric neutrinos on D 23 . We perform the global 3-analysis of the atmospheric and reactor neutrino data taking into account the effects of both the oscillations driven by the solar parameters (m 2 21 and 12 ) and the 1-3 mixing. The departure from the one-dominant mass scale approximation results into the shift of the 2 -3 mixing from maximal by sin 2 23 0:04, so that D 23 0:04 0:07 1. Though the value of the shift is not statistically significant, the tendency of the allowed region to move towards smaller values of sin 2 23 is robust. The shift is induced by the excess of the e-like events in the sub-GeV sample. We show that future large scale water Cherenkov detectors can determine D 23 with accuracy of a few percent, comparable with the sensitivity of future long-baseline experiments. Moreover, the atmospheric neutrinos will provide unique information on the sign of the deviation (octant of 23 ).