“…An estuarine plume is commonly observed to incline itself to either side of the coast, the Coriolis force as a driving factor, more typically against the coast to the right, facing downstream in the northern hemisphere [21]. Dynamics of the estuarine river plumes have been extensively studied through field observation [1,5,9,12,22,26,34,35,40,60,63,66,76,82], theoretical study [13,14,31,32,39,57,58,88], and numerical modeling [3, 4, 10, 11, 16-20, 28, 36, 37, 41, 43, 49, 54, 62, 64, 65, 70, 84, 89-93, 98, 99]. There has been considerable work done to understand how plume scales (along and across shore) depend on river discharge, as well as the importance of tides in modifying the plume dynamics.…”