The linear stability of a shear layer in a highly diffusive stably stratifi
ed atmosphere has been investigated. This study completes and extends previ
ous works by Dudis (1974) and Jones (1977). We show that (i) an asymptotic
regime is reached in the limit of large thermal diffusivity, (ii) there exi
sts two different types of unstable modes. The slowest growing modes corres
pond to predominantly horizontal motions and the fast growing ones to isotr
opic motions, (iii) the physical interpretation of the stability properties
in this asymptotic regime is simple. Applications to the dynamics of stell
ar radiative zone are discussed.