  This paper studies the d-dimensional (d=2,3) tropical climate model with only
the dissipation of the first baroclinic model of the velocity ($-\eta\Delta
v$). By choosing a class of special initial data $(u_0,v_0,\theta_0)$ whose
$H^s(\mathbb{R}^d)$ norm can be arbitrarily large, we obtain the global smooth
solution of d-dimensional tropical climate model.

Analysis of PDEs