Scientists have long understood that powerful undersea flows known as turbidity currents can alter ocean floors and damage critical cables that support global internet traffic. However, the precise mechanisms of their formation and behavior have remained largely elusive until now.
A recent study, spearheaded by an international team from Tsinghua University, has revealed that these potent currents are significantly more prevalent than previously assumed. The research indicates that these flows can originate in seemingly gentle environments, such as reservoirs and lakes, challenging the long-held belief that such currents were confined to more extreme submarine settings.
The findings, coupled with a newly developed framework for understanding turbidity current formation, are expected to enhance the ability to predict and manage these powerful natural phenomena. This improved understanding could lead to better protection for vital underwater infrastructure, including intercontinental telecommunication cables, and aid in the management of reservoirs.
In a paper published in the Proceedings of the National Academy of Sciences, the researchers described self-accelerating turbidity currents as formidable, erosive gravity underflows. They noted that despite progress in small-scale experimental setups, field observations of these accelerating currents have been rare, with most documented cases occurring in submarine environments.