A recent study conducted by Greenberg and Ganti examined the dynamics of river migration rates. The researchers gathered data from existing measurements of river migration rates and collected additional information from approximately 60 rivers, resulting in a total of 139 meandering rivers worldwide. These rivers varied in regions, climates, sizes, and vegetation regimes.
To track how river channels shifted over time, the researchers utilized satellite imagery to model each river segment as a series of line segments. This allowed them to measure the river’s migration rate.
Experimental evidence has shown that both vegetation and sediment load can play a role in slowing down river migration. However, the results of the study revealed that sediment load had a more significant impact on river migration rates than previously thought. Specifically, rivers with high sediment loads relative to their size migrated faster than those with lower sediment loads.
While vegetation did slow down river migration as previous studies suggested, its impact was more modest than initially believed. Unvegetated rivers migrated four times faster than similar-sized counterparts, rather than the reported 10-fold increase. This indicates that bar push rather than bank pull has a stronger influence on meandering rivers.
The study highlights that the behavior of a river is determined by the interaction between two processes: bar push and bank pull. In meandering rivers, one process cannot dominate the other. If there is not enough sediment supply, bank pull will outpace bar push, leading to a braided river. Therefore, it is the balance between these two processes that creates stable meandering rivers.