Local flow dynamics play a central role in physiological processes like respiration and nutrient uptake in coral reefs. Despite the importance of corals as hosts to a quarter of all marine life, and the pervasive threats currently facing corals, little is known about the detailed hydrodynamics of branching coral colonies. Here, in order to investigate the effects of the colony branch density and surface roughness on the local flow field, three-dimensional simulations were performed using immersed boundary, large-eddy simulations for four different colony geometries under low and high unidirectional oncoming flow conditions. The first two colonies were from the Pocillopora genus, one with a densely branched geometry, and one with a comparatively loosely branched geometry. The second pair of colony geometries were derived from a scan of a single Montipora capitata colony, one with the verrucae covering the surface intact, and one with the verrucae removed. We found that the mean velocity profiles in the densely branched colony changed substantially in the middle of the colony, becoming significantly reduced at middle heights where flow penetration was poor, while the mean velocity profiles in the loosely branched colony remained similar in character from the front to the back of the colony, with no middle-range velocity deficit appearing at the center of the colony. When comparing the turbulent flow statistics at the surface of the rough and smooth M. capitata colonies, we found higher Reynolds stress components for the smooth colony, indicating higher rates of mixing and transport compared to the rough colony, which must sacrifice mixing and transport efficiency in order to maintain its surface integrity in its natural high-flow environment. These results suggest that the densely branched, roughly patterned corals found in high flow areas may be more resistant not only to breakage, but also to flow penetration. motions transport planktonic food to the reef, while diffusion [3,4] takes place at a 6 much smaller scale at the coral surface. For the smaller scale processes, experimental 7 studies [5,6] show that growth direction, dimensions, and sparsity of branches depend 8 on the flow profile inside the coral [7][8][9]. Similarly, the velocity profile controls the 9 nutrient distribution [7,[10][11][12][13]. and physiological processes like photosynthesis and 10 respiration [14-17] near the coral surface. Flow motion also controls the thermal 11 micro-environment [18,19] at the coral surface, which is extremely important for 12 incidents like coral bleaching. Both the transfer of nutrients from the water column to 13 the coral and the transfer of byproducts from the coral to the water column depend on 14 the details of the flow through and around the coral [20, 21]. It is clear from the 15 discussion that all of these physical parameters are directly related to the flow 16 conditions in and around the coral geometry. To obtain a clear picture of this 17 interdependent relationship, the authors tried to find answers ...