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Exploring historical changes in mountain river hydrodynamics induced by human impact. | LitMetric

AI Article Synopsis

  • - The study investigates how human impacts have altered the channel morphology and hydrodynamics of the Czarny Dunajec River in Poland from 1964 to 2012 by analyzing archival aerial photos and using hydraulic modeling.
  • - Key findings indicate significant increases in water depth, flow velocity, and sediment characteristics during the flood scenarios between 1964 and 1983, with the largest floods showing the most dramatic changes, while later years (1983-2012) displayed less pronounced variations.
  • - The research highlights that understanding the historical hydrodynamics provides better insights into the river's response to floods and the ecological consequences of human-induced changes, rather than just assessing its current state.

Article Abstract

During the 20th-century many mountain rivers in Europe were subjected to intensive human impacts which substantially modified their channel morphology. How these changes affected river hydrodynamics and response to floods remains uncertain. In this work, we perform hydraulic modelling using data from archival aerial photos to explore relations between hydraulic parameters of floods and human-induced channel incision occurring on the Czarny Dunajec River (Polish Carpathians) between 1964 and 2012. Data on vertical position of the channel used for two-dimensional modelling of flood flows were extracted (as Digital Elevation Models DEMs) from archival aerial photos from 1964 and 1983 and ALS (Airborne Laser Skanning)-derived DEM from 2012. Water depth, flow velocity, bed shear stress, and sediment critical diameter were modelled for four flood scenarios (2-year, 5-year, 20-year, and 50-year floods) as well as the extent of flooded area and additionally the grain size of channel sediment was calculated. The values of water depth, flow velocity, bed shear stress and sediment critical diameter increased significantly between 1964 and 1983, especially for 20-year and 50-year floods. Only the flow velocity within the floodplain zone did not increase for the two largest flood scenarios due to the expansion of riparian forest in the second half of the twentieth century. The increase in flow rate was accompanied by a progressive reduction of the extent of flooded area, especially between 1964 and 1983, as well as by increase in mean grain size of channel sediment. Between 1983 and 2012 changes in hydraulic parameters were less pronounced, and coarser and well packed channel sediment dominated on the river bed. Our work demonstrates that reconstruction of past river hydrodynamics, rather than river state at time horizons, can give essential insights into functioning of the river channel and floodplain during the intensification of human impacts after 1950s.

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Source
http://dx.doi.org/10.1016/j.scitotenv.2024.174742DOI Listing

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