The lower-hybrid drift instability is simulated in an ion-scale current sheet using a fully kinetic approach with values of the ion to electron mass ratio up to m i =m e 1836. Although the instability is localized on the edge of the layer, the nonlinear development increases the electron flow velocity in the central region resulting in a strong bifurcation of the current density and significant anisotropic heating of the electrons. This dramatically enhances the collisionless tearing mode and may lead to the rapid onset of magnetic reconnection for current sheets near the critical scale. DOI: 10.1103/PhysRevLett.93.105004 PACS numbers: 52.35.Vd, 52.35.Kt, 94.30.Ej, 94.30.Gm Current sheets with characteristic thickness of the order of a thermal ion gyroradius i are routinely observed in Earth's magnetosphere [1,2] and within laboratory experiments designed to examine the physics of magnetic reconnection [3], a topic with widespread application to space, astrophysical, and laboratory plasmas. Although current sheets are unstable to a variety of plasma instabilities including collisionless tearing [4] and the lower-hybrid drift instability [5], the relative importance of these instabilities to the onset and development of large scale magnetic reconnection remains controversial.The lower-hybrid drift instability (LHDI) is driven by the diamagnetic current in the presence of inhomogeneities in the density and magnetic field [6]. The LHDI has been considered extensively as a possible candidate to modify the reconnection physics through anomalous resistivity generated by wave particle interactions [5,7,8]. Unfortunately, theory predicts the fastest growing modes with a wavelength on the electron gyroscale k y e 1 are localized on the edge of the layer [5], while enhanced fluctuations are required in the central region to produce significant anomalous resistivity. This conclusion is supported by observations at the magnetopause [9], in the magnetotail [10], and by laboratory experiments [11].Based on this evidence, some researchers have concluded the LHDI does not play an important role in current sheet dynamics. However, new results from both theory and simulation are beginning to challenge this conclusion. In a number of simulations, a strong enhancement of the central current density associated with the LHDI is observed [12 -16] and it has been suggested this effect gives rise to the rapid onset of reconnection [14,15]. Most of these simulations were performed with artificial ion to electron mass ratios m i =m e 100-400 and very thin layers i =L 1:7-2:2, where L is the half thickness of the layer. Although the simulations in Ref.[13] considered thicker layers at realistic mass ratio, the focus was on long wavelength effects, and the spatial resolution was insufficient to resolve the full LHDI spectrum.The very thin layers considered in most of the simulations are comparable in thickness to laboratory reconnection experiments [3,17] but are considerably thinner than observed in the magnetotail prior to onset. In ...