Air mass origin signals in δ 18 O of tree-ring cellulose revealed by back-trajectory modeling at the monsoonal Tibetan plateau

A profound consideration of stable oxygen isotope source water origins is a precondition for an unambiguous palaeoenvironmental interpretation of terrestrial δ O archives. To stress the influence of air mass origins on widely used δ O tree-ring chronologies, we conducted correlation analyses between...

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Published inInternational journal of biometeorology Vol. 61; no. 6; pp. 1109 - 1124
Main Authors Wernicke, Jakob, Hochreuther, Philipp, Grießinger, Jussi, Zhu, Haifeng, Wang, Lily, Bräuning, Achim
Format Journal Article
LanguageEnglish
Published United States 01.06.2017
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Summary:A profound consideration of stable oxygen isotope source water origins is a precondition for an unambiguous palaeoenvironmental interpretation of terrestrial δ O archives. To stress the influence of air mass origins on widely used δ O tree-ring chronologies, we conducted correlation analyses between six annually resolved δ O tree-ring cellulose ([Formula: see text]) 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 O values ([Formula: see text]) 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 [Formula: see text] 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 [Formula: see text] archives is better recorded at semi-humid sites.
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ISSN:0020-7128
1432-1254
DOI:10.1007/s00484-016-1292-y