noun A downward-growing, hollow tube of ice found in polar seas, formed by the release of cold, saline water from sea ice
In marine biology, a brinicle is a downward-growing hollow tube of ice enclosing a plume of cold brine that forms beneath sea ice. It is also known as an ice stalactite.
In oceanography, brinicles are important for understanding the freezing processes in polar oceans and their impact on marine life.
In climate science, brinicles play a role in the study of sea ice formation and its influence on global climate patterns.
A writer may use the term 'brinicle' in a science fiction story to describe a fictional phenomenon or as a metaphor for something destructive or chilling.
An oceanographer may use the term 'brinicle' to refer to a specific type of underwater icicle that forms beneath sea ice and has unique properties and implications for marine ecosystems.
A marine biologist may study the effects of brinicles on marine life and ecosystems, including how they can create microhabitats and impact the distribution of species in polar regions.
A climate scientist may research the formation and impact of brinicles as part of studying the changing dynamics of polar regions and their contribution to global climate patterns.