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favors the development of mixed-wave instability, with possible wave instability taking place first in the vicinity of the RMV. One can see from Eq. (14) that Q < 0 occurs in the eyewall mainly because of the presence of large vorticity (or PV) gradients and divergence (or small equivalent depth), suggesting that mixed-wave instability differs from algebraic instability for VRWs discussed by Nolan and Montgomery (2000) and Nolan et al. (2001) . Thus, we may state that intense convection in the
favors the development of mixed-wave instability, with possible wave instability taking place first in the vicinity of the RMV. One can see from Eq. (14) that Q < 0 occurs in the eyewall mainly because of the presence of large vorticity (or PV) gradients and divergence (or small equivalent depth), suggesting that mixed-wave instability differs from algebraic instability for VRWs discussed by Nolan and Montgomery (2000) and Nolan et al. (2001) . Thus, we may state that intense convection in the
