He correctly connected the appearance of secondary flow (both Earth atmosphere and tea cup) with "friction on the bottom".
[2] The formation of secondary flows in an annular channel was theoretically treated by Joseph Valentin Boussinesq as early as in 1868.
[1] The solution first came from Albert Einstein in a 1926 paper in which he explained the erosion of river banks and repudiated Baer's law.
[4][5] The stirring makes the water spin in the cup, causing a centrifugal force outwards.
[5] The phenomenon has been used to develop a new technique to separate red blood cells from blood plasma,[6][7] to understand atmospheric pressure systems,[8] and in the process of brewing beer to separate out coagulated trub in the whirlpool.