EGU24-15660, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-15660
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Machine learning analysis for predicting spatial distribution and key influencers of stable isotope patterns in European precipitation

Dániel Erdélyi1,2, Zoltán Kern1, István Gábor Hatvani1, Polona Vreča3, Klara Žagar3, Frederic Huneau4, Aurel Perșoiu5,6, Markus Leuenberger7,8, Sonja Lojen3, Oliver Kracht9, Astrid Harjung9, Pekka Rossi10, Kaisa-Riikka Mustonen11, and Jeffrey Welker11,12,13
Dániel Erdélyi et al.
  • 1Institute for Geological and Geochemical Research, HUN-REN Research Centre for Astronomy and Earth Siences, Budapest, Hungary (danderdelyi@gmail.com, zoltan.kern@gmail.com, hatvaniig@gmail.com)
  • 2Department of Geology, Eötvös Loránd University, Budapest, Hungary (danderdelyi@gmail.com)
  • 3Jožef Stefan Institute, Department of Environmental Sciences, Ljubljana, Slovenia (polona.vreca@ijs.si, klara.nagode@ijs.si, sonja.lojen@ijs.si)
  • 4Laboratoire d'Hydrogéologie CNRS UMR 6134 SPE, University of Corsica, Corte, France (huneau@univ-corse.fr)
  • 5Emil Racoviță Institute of Speleology, Romanian Academy, Cluj-Napoca, Romania (aurel.persoiu@gmail.com)
  • 6Stable Isotope Laboratory, Ștefan cel Mare University, Suceava, Romania (aurel.persoiu@gmail.com)
  • 7Climate and Environmental Physics, University of Bern, Bern, Switzerland (leuenberger@climate.unibe.ch)
  • 8Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland (leuenberger@climate.unibe.ch)
  • 9International Atomic Energy Agency, Department of Nuclear Sciences and Applications, Vienna, Austria (o.kracht@iaea.org, a.harjung@iaea.org)
  • 10Water Resources and Environmental Engineering Research Unit, University of Oulu, Oulu, Finland (pekka.rossi@oulu.fi)
  • 11Ecology and Genetics Research Unit, University of Oulu, Oulu, Finland (kaisa-eiikka.mustonen@oulu.fi, jeffrey.welker@oulu.fi)
  • 12Department of Biological Sciences, University of Alaska, Anchorage, United States (jmwelker@alaska.edu)
  • 13Ecology and Genetics Research Unit, University of the Arctic, Rovaniemi, Finland (jmwelker@alaska.edu)

Natural abundance variations in stable isotope ratios of hydrogen and oxygen are important environmental tracers with a significant range of applications  (e.g., the exploration of the present water cycle, paleoclimate reconstructions, ecology, and food authenticity). These applications and research themes are often based on spatially explicit predictions of precipitation isotopic variations obtained from point sample collections and measurements through various interpolation techniques. The derivation of spatially continuous and georeferenced isotope databases, known as isotopic landscapes (isoscapes), has been considered most effective through regression kriging for precipitation beginning in the early 2000s. However, the number of interpolation methods used in geostatistics has increased rapidly in recent decades, with new machine learning algorithms becoming increasingly important and proving more successful than conventional methods for certain isotopic parameters. In the present research we present a monthly 10 x 10 km European isoscape based on state-of-the art hybrid machine learning method that combines LASSO Regression and Random Forest (Zhang et al., 2019) for spatial predictions for 1973-2022. Data were retrieved from the IAEA/WMO Global Network of Isotopes in Precipitation (no. of stations: 329) and other national datasets from about 10 countries (no. of stations: ~150).

A pilot study (for 2008-2017; Erdélyi et al. 2023) indicated the highest prediction error for the northern premises. This suggested the incorporation of sea ice as an additional predictor, since a Pan-Arctic precipitation stable isotope study pointed out that sea ice cover change is a key driver of oceanic moisture sources (Mellat et al., 2021). Results indicate an overwhelming importance of minimum temperature with the variable representing sea ice cover, ranking among the least influential parameters. The analysis fails to consider moisture source effects, transport distances, and secondary processes of recycling associated with evaporation and transpiration from landscapes across Europe. These results provide a more refined prediction due to the higher station density compared to previous models and thanks to the hybrid model, a more accurate prediction of monthly precipitation stable isotope compositions is expected for the critical areas including the latitudinal margins as well as the mountainous zones.

Activities for this presentation were supported by the IAEA (CRP F31006, CRP F33024, TC-project RER7013, Contract 23550/R0) and WATSON Cost Action 19120. This research was also funded by UEFISCDI Romania, grants number PN-III-P2-2.1-PED-2019-4102, PN-III-P4-ID-PCE-2020-2723 and ARIS (Grants P1-0143, N1-0054, N1-0309, J6-3141, J6-50214).

 

Erdélyi, D., Kern, Z., Nyitrai, T., et al. (2023). Predicting the spatial distribution of stable isotopes in precipitation using a machine learning approach: a comparative assessment of random forest variants. International Journal of Geomathematics, 14:14. doi:10.1007/s13137-023-00224-x

Mellat, M., Bailey, H., Mustonen, K-R., Marttila, H., Klein, E. S., Gribanov, K., ... Welker, J. M. (2021). Hydroclimatic Controls on the Isotopic (δ18 O, δ2 H, d-excess)  Traits of Pan-Arctic Summer Rainfall Events. Frontiers in Earth Science, 9:651731. doi:10.3389/feart.2021.651731

Zhang, H., Nettleton, D., & Zhu, Z. (2019). Regression-enhanced random forests. arXiv preprint arXiv:1904.10416.

How to cite: Erdélyi, D., Kern, Z., Hatvani, I. G., Vreča, P., Žagar, K., Huneau, F., Perșoiu, A., Leuenberger, M., Lojen, S., Kracht, O., Harjung, A., Rossi, P., Mustonen, K.-R., and Welker, J.: Machine learning analysis for predicting spatial distribution and key influencers of stable isotope patterns in European precipitation, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-15660, https://doi.org/10.5194/egusphere-egu24-15660, 2024.

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