Skip to main content

Research Repository

Advanced Search

Temporal trends in δ18O composition of precipitation in Germany: Insights from time series modelling and trend analysis

Klaus, Julian; Chun, Kwok Pan; Stumpp, Christine

Authors

Julian Klaus

Profile Image

Dr Kwok Chun Kwok.Chun@uwe.ac.uk
Lecturer in Environmental Managment

Christine Stumpp



Abstract

Temporal and spatial variations of stable oxygen (18O) and hydrogen (2H) isotope measurements in precipitation act as important proxies for changing hydro-meteorological and regional and global climate patterns. Temporal trends in time series of the stable isotope composition in precipitation were rarely observed, and they are poorly understood. These might be a result of a lack of proper trend detection tools and effort for exploring trend processes. Here, we investigate temporal trends of δ18O in precipitation at 17 observation stations in Germany between 1978 and 2009. We test if significant trends in the isotope time series from different models can be observed. Mann-Kendall trend tests are applied on the isotope series, using general multiplicative seasonal autoregressive integrate moving average (ARIMA) models, which account for first and higher order serial correlations. Effects of temperature, precipitation, and geographic parameters on isotope trends are also investigated in the proposed models. To benchmark our proposed approach, the ARIMA results are compared with a trend-free pre-whitening procedure, the state of the art method for removing the first order autocorrelation in environmental trend studies. Moreover, we further explore whether higher order serial correlations in isotope series affects our trend results. Overall, three out of the 17 stations show significant changes when higher order autocorrelation are adjusted, and four show a significant trend when temperature and precipitation effects are considered. The significant trends in the isotope time series generally occur only at low elevation stations. Higher order autoregressive processes are shown to be important in the isotope time series analysis. Results suggest that the widely used trend analysis with only the first order autocorrelation adjustment may not adequately take account of the high order autocorrelated processes in the stable isotope series. The investigated time series analysis method including higher autocorrelation and external climate variable adjustments is shown to be a better alternative.

Citation

Klaus, J., Chun, K. P., & Stumpp, C. (2015). Temporal trends in δ18O composition of precipitation in Germany: Insights from time series modelling and trend analysis. Hydrological Processes, 29(12), 2668-2680. https://doi.org/10.1002/hyp.10395

Journal Article Type Article
Acceptance Date Oct 28, 2014
Online Publication Date Dec 3, 2014
Publication Date Jun 15, 2015
Deposit Date Jun 16, 2022
Journal Hydrological Processes
Print ISSN 0885-6087
Electronic ISSN 1099-1085
Publisher Wiley
Peer Reviewed Peer Reviewed
Volume 29
Issue 12
Pages 2668-2680
DOI https://doi.org/10.1002/hyp.10395
Keywords stable isotopes; precipitation; trend test; Mann–Kendall test; autocorrelation; ARIMA
Public URL https://uwe-repository.worktribe.com/output/9431564
Publisher URL https://onlinelibrary.wiley.com/doi/10.1002/hyp.10395