Abstract
A profound consideration of stable oxygen isotope source water origins is a precondition for an unambiguous palaeoenvironmental interpretation of terrestrial δ 18O archives. To stress the influence of air mass origins on widely used δ 18O tree-ring chronologies, we conducted correlation analyses between six annually resolved δ 18O tree-ring cellulose (\(\delta ^{18}\textit {O}_{TC}\)) chronologies and mean annual air package origins obtained from backward trajectory modeling. This novel approach has been tested for a transect at the southeastern Tibetan plateau (TP), where air masses with different isotopic composition overlap. Detailed examinations of daily precipitation amounts and monthly precipitation δ 18O values (\(\delta ^{18}\textit {O}_{P}\)) were conducted with the ERA Interim and Laboratoire de Météorologie Dynamique General Circulation Model (LMDZiso) data, respectively. Particularly the southernmost study sites are influenced by a distinct amount effect. Here, air package origin \(\delta ^{18}\textit {O}_{TC}\) relations are generally weaker in contrast to our northern located study sites. We found that tree-ring isotope signatures at dry sites with less rain days per year tend to be influenced stronger by air mass origin than tree-ring isotope values at semi-humid sites. That implies that the local hydroclimate history inferred from \(\delta ^{18}\textit {O}_{TC}\) archives is better recorded at semi-humid sites.
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The authors thank the German Federal Ministry of Education and Research (BMBF: FKZ 03G0811) and the German Research Council (DFG: BR 1895/21) for their financial support. We also thank Roswitha Höfner-Stich for her efficient and precise analysis of stable oxygen isotopes ratios in tree-ring cellulose. Additionally, we thank Dr. Masaki Sano for providing the data of study site Bhutan.
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Wernicke, J., Hochreuther, P., Grießinger, J. et al. Air mass origin signals in δ 18O of tree-ring cellulose revealed by back-trajectory modeling at the monsoonal Tibetan plateau. Int J Biometeorol 61, 1109–1124 (2017). https://doi.org/10.1007/s00484-016-1292-y
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DOI: https://doi.org/10.1007/s00484-016-1292-y