Finite-volume central-upwind schemes for shallow water equations were proposed in [A. Kurganov and G. Petrova, Commun. Math. Sci., 5 (2007), 133-160]. These schemes are capable of maintaining "lake-at-rest" steady states and preserving the positivity of the computed water depth. The well-balanced and positivity preserving features of the central-upwind schemes are achieved, in particular, by using continuous piecewise linear interpolation of the bottom topography function. However, when the bottom function is discontinuous or a model with a moving bottom topography is studied, the continuous piecewise linear approximation may not be sufficiently accurate and robust. In this paper, we modify the central-upwind scheme by approximating the bottom topography function using a discontinuous piecewise linear reconstruction (the same approximation used to reconstruct evolved quantities in the finite-volume setting) as well as implementing a special quadrature for the geometric source term and draining time step technique. We prove that the new central-upwind scheme possesses the wellbalanced and positivity preserving properties and illustrate its performance on a number of numerical examples. Keywords: hyperbolic system of conservation and balance laws, semi-discrete centralupwind scheme, Saint Venant system of shallow water equations.Mathematical subject classification: 76M12, 65M08, 35L65, 86-08, 86A05.