Changes between the active channel planform features of the lower Peiros River in 1945 and 2018 were examined through a multitemporal analysis performed in a GIS environment. The active channel experienced a consistent and rather generalized narrowing process (overall 71.6%, up to 84.3% at the reach-scale) along with localized increases of sinuosity and channel pattern variations associated with the disappearance of secondary channels and bars. Negligible changes in length occurred but the river mouth retreated by approximately 160 m. Large riverine areas disconnected from the active channel were involved in a peri-urbanization process and, thus, occupied by human activities and infrastructures; this resulted in anthropogenic landform modelling and increase in vulnerable elements exposed to hydrogeomorphic hazards. The observed active-channel planform changes could be, at least partly, human-induced. Further research is needed to define the Peiros River geomorphological evolution. The outcomes from this study represent an essential preliminary knowledge base under a river management perspective.
Channel planform changes on the lower Peiros River (Patras, Greece): 1945-2018 comparison
Mandarino, Andrea;Brandolini, Pierluigi
2022-01-01
Abstract
Changes between the active channel planform features of the lower Peiros River in 1945 and 2018 were examined through a multitemporal analysis performed in a GIS environment. The active channel experienced a consistent and rather generalized narrowing process (overall 71.6%, up to 84.3% at the reach-scale) along with localized increases of sinuosity and channel pattern variations associated with the disappearance of secondary channels and bars. Negligible changes in length occurred but the river mouth retreated by approximately 160 m. Large riverine areas disconnected from the active channel were involved in a peri-urbanization process and, thus, occupied by human activities and infrastructures; this resulted in anthropogenic landform modelling and increase in vulnerable elements exposed to hydrogeomorphic hazards. The observed active-channel planform changes could be, at least partly, human-induced. Further research is needed to define the Peiros River geomorphological evolution. The outcomes from this study represent an essential preliminary knowledge base under a river management perspective.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.