“…Another example is the following wave equation which is damped on one half of its rectangular domain but not on the other: Here Ω = (−1, 1) × (0, 1) and Ω + = (0, 1) × (0, 1) as in Section 1, and u 0 , v 0 are suitable functions defined on Ω. In this case the energy E z 0 (t) = 1 2 Ω |∇u(x, y, t)| 2 + |u t (x, y, t)| 2 d(x, y), t ≥ 0, of any classical solution u, with corresponding initial data z 0 = (u 0 , v 0 ), can be shown to satisfy E z 0 (t) = o(t −4/3 ) as t → ∞, and furthermore this estimate is sharp; see [3, Part IV.B], [17] and also [11,15]. Our methods can also be adapted to study the following wave equation on the square Ω − = (−1, 0)× (0, 1) subject to Dirichlet boundary conditions along three of its edges but with the coupled heat equation in (1.1) replaced by a dissipative boundary condition along the fourth edge:…”