alikasvostoon

Alikasvostoon, also known as the "tail of the sea," is a phenomenon observed in the Baltic Sea, particularly in the Gulf of Finland. It refers to a large-scale, slow-moving vortex that forms in the sea's bottom layer, typically during the winter months. This vortex is characterized by its counter-clockwise rotation and can span several kilometers in diameter.

The formation of alikasvostoon is influenced by a combination of factors, including the shape of the Gulf of Finland, the influence of the Gulf Stream, and the seasonal changes in water temperature and salinity. The vortex is believed to be a result of the interaction between the warm, saline water from the Gulf Stream and the colder, fresher water from the Baltic Sea.

Alikasvostoon plays a significant role in the ecosystem of the Gulf of Finland. It helps to distribute nutrients and oxygen throughout the water column, supporting the growth of phytoplankton and other marine life. Additionally, the vortex can influence the distribution of fish and other marine organisms, as well as the transport of pollutants and other materials within the sea.

Despite its ecological importance, alikasvostoon is not well-studied, and much remains unknown about its formation, behavior, and impact on the marine environment. Ongoing research aims to better understand this fascinating and complex phenomenon, as well as its potential implications for the future of the Baltic Sea.