Question: What British physicist is a Taylor scraping flow named after?
Context: Prof Edward Taylor Jones FRSE LLD (1872-1961) was a British physicist.  He was Professor of Natural Philosophy at Glasgow University from 1925 to 1943. John Bryan Taylor (born 1928 in Birmingham) is a British physicist known for his important contributions to plasma physics and their application in the field of fusion energy.  Notable among these is the development of the "Taylor state", describing a minimum-energy configuration that conserves magnetic helicity.  Another important development was his work on the ballooning transformation, which describes the motion of plasma in toroidal (donut) configurations, which are widely used in the fusion field.  Taylor has also made important contributions to the theory of the Earth's Dynamo, including the famous Taylor constraint. In fluid dynamics, the Taylor–Green vortex is an unsteady flow of a decaying vortex, which has an exact closed form solution of the incompressible Navier–Stokes equations in Cartesian coordinates.  It is named after the British physicist and mathematician Geoffrey Ingram Taylor and his collaborator A. E. Green. A Kelvin–Voigt material, also called a Voigt material, is a viscoelastic material having the properties both of elasticity and viscosity.  It is named after the British physicist and engineer Lord Kelvin and after German physicist Woldemar Voigt. Sir Geoffrey Ingram Taylor OM (7 March 1886 – 27 June 1975) was a British physicist and mathematician, and a major figure in fluid dynamics and wave theory.  His biographer and one-time student, George Batchelor, described him as "one of the most notable scientists of this (the 20th) century". Montonen–Olive duality or electric-magnetic duality is the oldest known example of strong-weak duality or S-duality according to current terminology.  It generalizes the electro-magnetic symmetry of Maxwell's equations by stating that magnetic monopoles, which are usually viewed as emergent quasiparticles that are "composite" (i.e. they are solitons or topological defects), can in fact be viewed as "elementary" quantized particles with electrons playing the reverse role of "composite" topological solitons; the viewpoints are equivalent and the situation dependant on the duality.  It was later proven to hold true when dealing with a N = 4 supersymmetric Yang–Mills theory.  It is named after Finnish physicist Claus Montonen and British physicist David Olive after they proposed the idea in their academic paper "Magnetic monopoles as gauge particles? " where they state: In fluid dynamics, Taylor scraping flow is a type of two-dimensional corner flow occurring when one of the wall is sliding over the other with constant velocity, named after G. I. Taylor. Glen Peak ( ) is a peak on the north end of Liard Island in Hanusse Bay, Antarctica.  It was mapped from air photos obtained by the Ronne Antarctic Research Expedition (1947–48) and the Falkland Islands and Dependencies Aerial Survey Expedition (1956–57).  It was named by the UK Antarctic Place-Names Committee for John W. Glen, a British physicist who has made laboratory investigations on the flow of single and polycrystalline ice. The Taylor microscale, which is sometimes called the turbulence length scale, is a length scale used to characterize a turbulent fluid flow.  This microscale is named after Geoffrey Ingram Taylor.  The Taylor microscale is the intermediate length scale at which fluid viscosity significantly affects the dynamics of turbulent eddies in the flow.  This length scale is traditionally applied to turbulent flow which can be characterized by a Kolmogorov spectrum of velocity fluctuations.  In such a flow, length scales which are larger than the Taylor microscale are not strongly affected by viscosity.  These larger length scales in the flow are generally referred to as the inertial range.  Below the Taylor microscale the turbulent motions are subject to strong viscous forces and kinetic energy is dissipated into heat.  These shorter length scale motions are generally termed the dissipation range. The Stefan flow, occasionally called Stefan's flow, is a transport phenomenon concerning the movement of a chemical species by a flowing fluid (typically in the gas phase) that is induced to flow by the production or removal of the species at an interface.  Any process that adds the species of interest to or removes it from the flowing fluid may cause the Stefan flow, but the most common processes include evaporation, condensation, chemical reaction, sublimation, ablation, adsorption, absorption, and desorption.  It was named after the Austrian physicist, mathematician, and poet Josef Stefan for his early work on calculating evaporation rates.
Answer: G. I. Taylor