In this paper, we consider the 3D tropical climate model with damping terms in the equation of u, v and θ\documentclass[12pt]{minimal}
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\begin{document}$$\theta $$\end{document}, respectively. Firstly, we get some uniform estimates of strong solution. Secondly, we derive the result of the continuity of the semigroup {S(t)}t≥0\documentclass[12pt]{minimal}
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\begin{document}$$\{S(t)\}_{t\ge 0}$$\end{document} in case of 4≤α,β<5\documentclass[12pt]{minimal}
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\begin{document}$$4\le \alpha ,\beta <5$$\end{document} and 135<γ<5\documentclass[12pt]{minimal}
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\begin{document}$$\frac{13}{5}<\gamma <5$$\end{document} via some usual inequalities. Finally, the system (1.1) is shown to possess an (V,V)\documentclass[12pt]{minimal}
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\begin{document}$$({\mathbb {V}},{\mathbb {V}})$$\end{document}-global attractor and an (V,H2)\documentclass[12pt]{minimal}
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\begin{document}$$({\mathbb {V}},{\textbf{H}}^{2})$$\end{document}-global attractor.