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We prove local well-posedness for the gravity water waves equations without surface tension, with initial velocity field in , $s > \frac{d}{2} + 1 - \mu\mu = \frac{1}{10}d = 1\mu = \frac{1}{5}$ in the case , extending previous results of Alazard-Burq-Zuily. The improvement primarily arises in two areas. First, we perform an improved analysis of the regularity of the change of variables from Eulerian to Lagrangian coordinates. Second, we perform a time-interval length optimization of the localized Strichartz estimates.

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