Meier WJH, Wernicke J, Huang R, Zhu H, Aryal S, Grießinger J (2026)
Publication Type: Journal article
Publication year: 2026
Book Volume: 256
Article Number: 105166
DOI: 10.1016/j.gloplacha.2025.105166
High-elevation dwarf shrubs above the Himalayan treeline offer a valuable but underexplored archive for paleoclimatic research. This study analyses the stable oxygen isotope composition (δ18O) of Juniperus indica dwarf shrub-rings collected above 4000 m a.s.l. on the southern flank of the Himalayan Arc to evaluate their sensitivity to climatic variability. The δ18O series demonstrates a clear and coherent response to hydroclimatic conditions during the core summer monsoon season. Daily synoptic-scale analysis reveals that break monsoon weather patterns, rather than active monsoon phases, are the primary drivers of isotopic variability. Break phases are linked either to enhanced northwesterly airflow, leading to suppressed precipitation, or to a northward displacement of the monsoon trough, intensifying precipitation across the Himalayan Arc. Backward air mass trajectory modelling, combined with outgoing longwave radiation data reveal that isotopically enriched δ18O values correspond to westerly advection under reduced convective activity, whereas depleted δ18O values coincide with enhanced southerly flow and stronger convective activity. Collectively, these synoptic-scale circulation patterns explain up to 30 % of the observed δ18O variance. Our findings highlight the central role of break monsoon dynamics in shaping cellulose δ18O variability and demonstrate the potential of high-elevation dwarf shrubs as proxies for synoptic-scale paleoclimate in the Himalayas
APA:
Meier, W.J.H., Wernicke, J., Huang, R., Zhu, H., Aryal, S., & Grießinger, J. (2026). Beyond the treeline: assessing the potential of juniper shrub-ring δ18O for paleoclimatic research in the Himalayas. Global and Planetary Change, 256. https://doi.org/10.1016/j.gloplacha.2025.105166
MLA:
Meier, Wolfgang Jens Henrik, et al. "Beyond the treeline: assessing the potential of juniper shrub-ring δ18O for paleoclimatic research in the Himalayas." Global and Planetary Change 256 (2026).
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