EGU2020-5871
https://doi.org/10.5194/egusphere-egu2020-5871
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Climate change reshapes the drivers of false spring risk across European trees

Catherine Chamberlain1,2, Benjamin Cook3, Ignacio Morales-Castilla4,5, and Elizabeth Wolkovich1,2,6
Catherine Chamberlain et al.
  • 1Arnold Arboretum of Harvard University, Boston, Massachusetts, United States of America (cchamberlain@g.harvard.edu)
  • 2Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts, United States of America (cchamberlain@g.harvard.edu)
  • 3NASA Goddard Institute for Space Studies, New York, New York, United States of America
  • 4GloCEE - Global Change Ecology and Evolution Group, Department of Life Sciences, Universidad de Alcalá, Alcalá de Henares, Spain
  • 5Department of Environmental Science and Policy, George Mason University, Fairfax, Virginia, United States of America
  • 6Forest and Conservation Sciences, Faculty of Forestry, University of British Columbia, Vancouver, British Columbia, Canada

Temperate and boreal forests are shaped by late spring freezing events after budburst, which are also known as false springs. Research has generated conflicting results on whether or not these events will change with climate change, potentially because---to date---no study has compared the myriad climatic and geographic factors that contribute to a plant's risk of a false spring. We assessed and compared the strength of the effects of mean spring temperature, distance from the coast, elevation and the North Atlantic Oscillation (NAO) using PEP725 leafout data for six temperate, decidious tree species across 11,648 sites in Central Europe and how these predictors shifted with climate change. Across species before recent warming, mean spring temperature and distance from the coast were the strongest predictors, with higher mean spring temperatures associated with decreased risk in false springs (–7.64% per 2°C increase) and sites further from the coast experiencing an increased risk (5.32% per 150km from the coast). Elevation (2.23% per 200m increase in elevation) and NAO index (1.91% per 0.3 increase) also increased false spring risk. 

With climate change, elevation and distance from coast---i.e., the geographic factors---remain relatively stable, while climatic factors shifted in magnitude for mean spring temperature (down to -2.84% in risk per 2°C), and in direction, with positive NAO phases leading to lower risk (-9.15% per 0.3). The residual effects of climate change---unexplained by the climatic and geographic factors already included in the model---magnified the species-level variation in risk, with risk increasing among early-leafout species (i.e., Aesculus hippocastanum, Alnus glutinosa and Betula pendula) but a decline or no change in risk among late-leafout species (i.e., Fagus sylvatica, Fraxinus excelsior and Quercus robur). Our results show that climate change has reshaped the major drivers of false spring risk and highlight how considering multiple factors can yield a better understanding of the complexities of climate change.

How to cite: Chamberlain, C., Cook, B., Morales-Castilla, I., and Wolkovich, E.: Climate change reshapes the drivers of false spring risk across European trees, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5871, https://doi.org/10.5194/egusphere-egu2020-5871, 2020

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