EGU23-5744
https://doi.org/10.5194/egusphere-egu23-5744
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Quantification of the reasons for the bird lake brownification in Finland

Katri Rankinen1, Virpi Junttila1, Martyn Futter2, José Enrique Cano Bernal1, Daniel Butterfield3, and Maria Holmberg1
Katri Rankinen et al.
  • 1Finnish Environment Institute, Biodiversity Center, Helsinki, Finland (katri.rankinen@ymparisto.fi)
  • 2Swedish University of Agricultural Sciences
  • 3Other

Browning of surface waters due to increased terrestrial loading of dissolved organic carbon is observed across the Northern Hemisphere. Brownification is often explained by changes in large scale anthropogenic pressures (acidification, climate and land use). We quantified the effect of environmental changes on observed brownification of an important bird lake Kukkia in Central Finland. Water bird densities have decreased there during last decades, probably due to brownification of the lake. We studied past trends of organic carbon loading from catchments based on observations since 1990’s. We created scenarios for atmospheric deposition, climate and land use change to simulate their quantitative effect on brownification of the lake by process-based models (PERSiST for hydrology, INCA-C for carbon loading and MyLake for carbon processes in the lake). Increase in forest cut area appeared to be the primary reason for brownification of the lake. Decrease in acidic deposition has resulted in a lower leaching of dissolved organic carbon, but the effect is small. Runoff and total organic carbon leaching from terrestrial areas to the lake is smaller than it would have been without observed increasing trend in temperature by two degrees. 

How to cite: Rankinen, K., Junttila, V., Futter, M., Cano Bernal, J. E., Butterfield, D., and Holmberg, M.: Quantification of the reasons for the bird lake brownification in Finland, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-5744, https://doi.org/10.5194/egusphere-egu23-5744, 2023.