EGU21-11514
https://doi.org/10.5194/egusphere-egu21-11514
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Climate change effects on forest floor interception in woody Cerrado ecosystem

Livia Rosalem1, Miriam Gerrits-Coenders2, Jamil A. A. Anache3, Julian S. Sone1, Dimaghi Schwamback1, Alessandra Campos1, and Edson Wendland1
Livia Rosalem et al.
  • 1University of São Paulo, São Carlos School of Engineering, Hydraulics and Sanitation, São Carlos, Brazil (liviarosalem@gmail.com)
  • 2Delft University of Technology, Water Resources Section, Delft, the Netherlands
  • 3Federal University of Mato Grosso do Sul, Campo Grande, Brazil

The interception process is an important redistributor of water fluxes, which can considerably affect terrestrial evaporation. Not only the canopy intercepts water, but also from the forest floor significant amounts of water vapor return to the atmosphere. Remaining forests are important areas to evaluate the possible effects of climate change on the water partitioning process. Despite the hydrologic and ecosystem services offered by Cerrado forests, the interception process, as well as climate change threats on the evaporative flux of such forests, are still unknown. This study attempts to anticipate the possible impacts on the forest floor interception process in Cerrado stricto sensu considering future scenarios of climate change. To accomplish this, we used data of field monitoring from June 2017 to February 2020 in an undisturbed Cerrado s.s. forest in São Paulo State, Brazil. We calibrated and validated an improved version of the Rutter interception model (Rutter et al., 1971), which includes interception from the forest floor. Projected climate change scenarios were obtained from the National Institute for Space Research (INPE, Brazil) from 2006 to 2099 with 5km spatial resolution generated by Eta-HadGEM2-ES regional climate model under representative concentration pathway (RCP) 4.5. The results indicate increased rainfall and decreased potential evaporation in the decade 2041-2060. By the Rutter model, the total interception increased for this period (2041-2060) associated with decreased forest floor evaporation. During the first (2006-2020) and the last (2081-2099) decades, the predictions suggest an increase of 2.4% on the average annual percentage of forest floor evaporation, also an increase of minimum annual interception percentages (from 17.1% to 18.7%). Thus, our results demonstrate the relevance of forest floor to the interception process and suggest that it can be even more relevant in the future due to the climate changes.

How to cite: Rosalem, L., Gerrits-Coenders, M., A. A. Anache, J., S. Sone, J., Schwamback, D., Campos, A., and Wendland, E.: Climate change effects on forest floor interception in woody Cerrado ecosystem, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-11514, https://doi.org/10.5194/egusphere-egu21-11514, 2021.

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