👉 The gale fluid, also known as galea fluid or gust fluid, is a hypothetical substance proposed by some researchers to describe the complex interactions and energy exchanges occurring within the Earth's upper atmosphere, particularly in the boundary layer between the troposphere and the stratosphere. This fluid is theorized to represent the dynamic, turbulent flow of air masses, characterized by intense wind shear and high levels of kinetic energy. It encompasses the exchange of momentum, heat, and chemical species between different atmospheric layers, playing a crucial role in weather patterns and climate dynamics. However, it's important to note that while the concept of gale fluid is intriguing and has been proposed in various studies, it remains largely theoretical and not yet fully substantiated by empirical evidence.
