Jelaskan Subsidence inversion dari Penyongsangan suhu dalam bahasa melayu

An inversion can develop aloft as a result of air gradually sinking over a wide area and being warmed by adiabatic compression, usually associated with subtropical high-pressure areas. A stable marine layer may then develop over the ocean as a result. As this layer moves over progressively warmer waters, however, turbulence within the marine layer can gradually lift the inversion layer to higher altitudes, and eventually, even pierce it, producing thunderstorms, and under the right circumstances, leading to tropical cyclones.  The accumulated smog and dust under the inversion quickly taints the sky reddish, easily seen on sunny days.