EGU25-7260, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-7260
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 28 Apr, 16:15–18:00 (CEST), Display time Monday, 28 Apr, 14:00–18:00
 
Hall X5, X5.130
A long-term drought reconstruction based on oxygen isotope tree ring data for central and eastern parts of Europe (Romania)
Viorica Nagavciuc1,2, Gerhard Helle3, Maria Rădoane2, Cătălin-Constantin Roibu2, Mihai-Gabriel Cotos2, and Monica Ionita1,2
Viorica Nagavciuc et al.
  • 1Alfred Wegener Institute for Polar and Marine Research, Paleoclimate Dynamics, Suceava, Germany (nagavciuc.viorica@gmail.com)
  • 2Forest Biometrics Laboratory – Faculty of Forestry, “Stefan cel Mare” University of Suceava, Universit˘a¸tii Street No. 13, Suceava 720229, Romania
  • 3German Research Centre for Geosciences GFZ, 4.3 Climate Dynamics and Landscape Evolution, Telegrafenberg, Potsdam 14473, Germany

This study investigates the relationship between oxygen isotope ratios (δ¹⁸O) in oak tree ring cellulose and past drought variability in Letea Forest, Romania. A δ¹⁸O site chronology spanning 1803-2020 was compiled from seven individual time series. δ¹⁸O values exhibited a significant negative correlation with moisture-related variables (cloud cover, relative humidity, and precipitation) and a positive correlation with temperature and sunshine duration. This confirms that δ¹⁸O from tree rings can be a good proxy for moisture availability. The strongest correlation was found between δ¹⁸O and the August Standardized Precipitation Evapotranspiration Index for an accumulation period of 9-months (SPEI9) for central and eastern Europe. This highlights SPEI9 as a superior indicator of drought compared to individual parameters like temperature or precipitation. Using a linear regression model, we reconstructed August SPEI9 variability for the past 200 years. The reconstruction captured interannual and decadal variations, with distinct wet and dry periods. Analysis of large-scale atmospheric circulation patterns revealed a link between high δ¹⁸O values (indicating dry conditions) and a high-pressure system over the North Atlantic. Conversely, low δ¹⁸O values (indicating wet conditions) corresponded to negative pressure anomalies over Europe. Moreover, extreme values of δ¹⁸O are also associated with the prevalence of a hemispheric teleconnection pattern, namely wave number 4. This δ¹⁸O chronology and the corresponding August SPEI9 reconstruction offer valuable tools for understanding past climate variability and its relationship with large-scale atmospheric and oceanic circulation patterns.

How to cite: Nagavciuc, V., Helle, G., Rădoane, M., Roibu, C.-C., Cotos, M.-G., and Ionita, M.: A long-term drought reconstruction based on oxygen isotope tree ring data for central and eastern parts of Europe (Romania), Biogeosciences, 22, 55–69, https://doi.org/10.5194/bg-22-55-2025, 2025

Nagavciuc, V., Helle, G., Rădoane, M., Roibu, C.-C., Cotos, M.-G., and Ionita, M.: A long-term drought reconstruction (August SPEI9) based on oxygen isotope tree ring data for central and eastern parts of Europe (Romania), Zenodo [data set], https://doi.org/10.5281/zenodo.14536886, 2024.

How to cite: Nagavciuc, V., Helle, G., Rădoane, M., Roibu, C.-C., Cotos, M.-G., and Ionita, M.: A long-term drought reconstruction based on oxygen isotope tree ring data for central and eastern parts of Europe (Romania), EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-7260, https://doi.org/10.5194/egusphere-egu25-7260, 2025.