Pao-Hsing Chang

Learn More
The Northwestern Tropical Atlantic (NwTA) is one of the regions in the tropical oceans where thick barrier layers (BLs) form during boreal fall and winter. Once formed, BLs tend to inhibit entrainment cooling of the mixed layer. Compared to observations, many coupled General Circulation Models (GCMs) misrepresent the dynamics of BLs. It is shown that this(More)
  • 1