Jon Schwenk receives PhD for dissertation titled, "Meandering rivers: interpreting dynamics from planform geometry and the secret lives of migrating meanders"
PhD candidate Jon Schwenk successfully defended his dissertation in Civil, Environmental, and Geo-Engineering on Thursday, August 18th, 2016. He is advised by Professor Efi-Foufoula-Georgiou of the St. Anthony Falls Laboratory and the Department of Civil, Environmental, and Geo-Engineering. Jon was also SAFL's 2016 Alvin Anderson Award winner. Congratulations, Dr. Schwenk!!
Dissertation Title: Meandering rivers: interpreting dynamics from planform geometry and the secret lives of migrating meanders
Meandering rivers are dynamic agents of geomorphic change that rework landscapes through migration while maintaining beautiful looping planforms. This work investigates the relationships between the alluring planform geometries of meandering rivers, the dynamics of individual meander bend migration, and the dynamic processes driving meander evolution. A simple yet physically-based model of long-time meander migration is employed to understand the dynamic trajectories of individual meander bends and establish relationships between historic dynamics and cutoff bend geometry. At the reach scale, concepts from nonlinear dynamic theory are applied to river centerlines to determine if the dynamic nonlinearities driving meander evolution are preserved in the reachwide planform structure. Understanding how rivers move across their floodplains requires snapshots of planforms over long time periods from aerial photography or historic maps and surveys which are often taken at irregular and long intervals. Migration occurring between snapshots has thus largely remained a mystery. More recently, worldwide satellite imagery collected at least every 18 days by the NASA Landsat family of satellites offers the potential to reveal the secret lives of migrating, meandering rivers. This research mines the vault of Landsat imagery to resolve over 30 years of planform migration along more than 1,300 km of one of the Earth's most active meandering rivers: the Ucayali River in Peru. Analysis of the resulting annual binary channel masks suggests that migration rates are controlled by processes acting across bend-to-reach scales. An exciting new geomorphic discovery emerges from the analysis revealing the role of cutoffs as drivers of nonlocal morphodynamic change.