|Kelvin-Helmholtz Instability (KHI) is a hydrodynamic instability in which immiscible, incompressible, and inviscid fluids are in relative and irrotational motion. The basic mechanism of KHI development is in the existence of a uniform velocity shear and that does not need gravity or density difference. The horizontal boundary, corresponding to a sharp difference of velocity in the fluid is a shearing layer. Lighter layer of fluid floats over another, heavier layer (such as in a lake in summer). Physical principles tell us that gravity waves can propagate on the interface separating these two layers, not unlike waves propagating on the surface of a pond. But, if the layers flow at different velocities, i.e. when a shear is present, these waves may grow in time and lead to overturning in the vicinity of the interface. These breaking internal waves, called billows, generate mixing over a height a little shorter than their wavelength. The phenomenon is known as the Kelvin-Helmholtz instability.
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Journal of Vortex Science and Technology is one of the Open access peer-reviewed journal in the domain of Kelvin-Helmholtz Instability theory. The journals are regularly involved in publication of current research in the form of original research and reviews. The Editorial team of this journal includes globalized experts in the field of vortex science involved in regular review of submitted manuscripts facilitating high quality of articles since many years. Journals are the major sources of knowledge for young and aspiring generations who are keen to pursue a career in physics
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