Scaling arguments, based on non-dimensional parameters accounting for the surrounding flow characteristics and the geometry of the seamount, allow an estimate of the dynamical processes that may be active at the bank. Temporary Taylor cap formation by weak impinging flow may occur, although a clear signature of this feature does not emerge from the observed density fields. The strong local amplification of the diurnal tide suggests the presence of resonant seamount trapped waves. The strength of the semidiurnal tide in the region, in combination with the steepness of the flanks of the bank, points to a significant contribution of tidally rectified flow to the observed residual anticyclonic flow. An observation of an isopycnal vertically repositioned by 50 m within one downcast/upcast period of a CTD profile indicates the importance of high frequency internal wave dynamics.