A simple model for the eta(i)-mode taking account of the dissipative t
rapped electron effect, which is described by means of the well-known
formula of the nonadiabatic electron response, in a sheared slab geome
try is presented. It predicts the existence of a hybrid dissipative tr
apped electron ion temperature gradient (ITG) mode. This conclusion is
in agreement with the observation in the latest simulated tokamak exp
eriment on the Columbia Linear Machine.