Since the 1980s, subsurface temperature seasonality in extratropical oceans has decreased by 5.7 ± 1.8% below the mixed layer due to increased heat uptake from greenhouse gases, strengthening upper ocean stratification, and limiting heat penetration into deeper layers, according to analysis of a hierarchy of climate models and an idealized diffusive model.
- Fukai Liu
- Yiyong Luo
- Lijing Cheng