In a seminal paper, Paola (1996) put forward an analogy between river braiding and fluid turbulence. He observed that both fluid turbulence and river braiding form systems that: (a) are intrinsically unpredictable in their exact configurations in the long term despite being governed by deterministic laws that are reasonably well known; (b) feature a hierarchy of scales; and, (c) while they can be macroscopically stationary, feature transient events which are critical to the system's average behavior. From these observations, he proceeded to develop a one-dimensional analytical model for hydraulic geometry, shear stress and sediment transport in braided channels based on an adaptation of the Reynolds decomposition used in the turbulence theory, which aligned reasonably well with field data.To our knowledge, this turbulence analogy has not been developed or used further to interpret braiding. Yet, this framework could provide more, potentially ground-breaking insight into the nature and functioning of braiding by answering fundamental questions such as the existence of one (or multiple) scaling relations; the existence of a hierarchical structure where features of different sizes can be interpreted as being functionally different; the