Fractal characteristics of the middle reach of the Paraná River floodplain during extreme hydrological events

LUIS ALBERTO ESPINOLA; FEDERICO YOYA; DIEGO SKLAR; FÉLIX IGNACIO CONTRERAS; ELIE ABRIAL; ENRIQUE MARCELO ALBORNOZ; ALDO RAUL PAIRA; ANA PIA RABUFFETTI; MARTIN CESAR MARIA BLETTLER; HUGO AIMAR

RIVER RESEARCH AND APPLICATIONS

JOHN WILEY & SONS LTD

Lugar: LOndres; Año: 2023 p. 1 - 14

1535-1459

The hydrological events that occur on floodplains are largely defined by precipitation and runoff inputs interacting with their geomorphological characteristics. In the middle Paraná River (MPR), hydrological events have traditionally been studied using water level time series and topographic charts or satellite images of certain floodplain sectors, using the same scale throughout the study area. Different zones of the floodplain were integrated using fractal dimension (FD) to better understand hydrological processes. FD is a useful tool used to characterize the geomorphological complexity of river networks in watersheds. The box-counting method was applied in the MPRfloodplain. The result showed that as water levels increase, FD decreases, thereby indicating the direct relation with the hydrological attributes of the floodplain (e.g., duration, magnitude, recurrence of the flood event, and connectivity). This relation constitutes the basis of a new approach of the analysis of hydrological events and their effect on the MPR floodplain. This research provides fundamental information obtained from two hydrological stages and different spatial scales which may complement the method designed to accurately understand the hydrogeomorphological processes that operate on the Paraná River floodplain. It provides a simpleparameter that can be used to evaluate the role that each floodplain section plays in attenuating the hydrograph recorded at each gauge analyzed along the river. This information will be useful in the implementation of management policies directed to the mitigation of future hydrological threats generated by alterations in the hydrological regime due to hydroclimatic variations or watershed alterations. The results further strengthen the basis for integrated sustainable planning of the main channel of the Paraná River, its floodplain, and the resources provided by this ecosystem.