merikerrostumat
Merikerrostumat refers to the stratification of seawater into distinct layers based on differences in properties like temperature, salinity, and density. These layers are not static and can change over time due to various physical and chemical processes.
The most common stratification is driven by temperature. Warmer, less dense water tends to float on top
Salinity also plays a significant role in merikerrostumat. Areas with higher salinity have denser water and
These merikerrostumat are crucial for marine ecosystems. They influence the distribution of nutrients, oxygen, and marine