Atmospheric Physics
Rayleigh-Taylor instability is a phenomenon that occurs at the interface of two fluids with different densities when the lighter fluid is pushing into the heavier fluid under the influence of gravity. This instability can lead to the mixing of fluids and is important in understanding various atmospheric and astrophysical processes, such as those found in the ionosphere, where density differences play a crucial role in wave propagation and plasma dynamics.
congrats on reading the definition of Rayleigh-Taylor Instability. now let's actually learn it.