40 citations as recorded by crossref.

1. May–September precipitation in the Bhutan Himalaya since 1743 as reconstructed from tree ring cellulose δ18O M. Sano et al. 10.1002/jgrd.50664
2. Radial growth and climate responses of healthy versus decayed subalpine conifer trees in the southeastern Qinghai-Tibetan Plateau L. Luo et al. 10.1016/j.ecolind.2024.112845
3. Increased drought events in southwest China revealed by tree ring oxygen isotopes and potential role of Indian Ocean Dipole C. Xu et al. 10.1016/j.scitotenv.2019.01.186
4. Indian monsoon precipitation isotopes linked with high level cloud cover at local and regional scales D. Wang et al. 10.1016/j.epsl.2019.115837
5. Drought signals in tree-ring stable oxygen isotope series of Qilian juniper from the arid northeastern Tibetan Plateau C. Qin et al. 10.1016/j.gloplacha.2014.12.002
6. A 400-year tree-ring δ18O chronology for the southeastern Tibetan Plateau: Implications for inferring variations of the regional hydroclimate X. Liu et al. 10.1016/j.gloplacha.2013.02.005
7. Variability of summer humidity during the past 800 years on the eastern Tibetan Plateau inferred from δ<sup>18</sup>O of tree-ring cellulose J. Wernicke et al. 10.5194/cp-11-327-2015
8. Modelling tree ring cellulose <i>δ</i><sup>18</sup>O variations in two temperature-sensitive tree species from North and South America A. Lavergne et al. 10.5194/cp-13-1515-2017
9. The response of relative humidity to centennial-scale warming over the southeastern Tibetan Plateau inferred from tree-ring width chronologies C. Shi et al. 10.1007/s00382-018-4107-5
10. Hydroclimatic seasonality recorded by tree ring δ18O signature across a Himalayan altitudinal transect C. Brunello et al. 10.1016/j.epsl.2019.04.030
11. Tree-ring oxygen isotope across monsoon Asia: Common signal and local influence C. Xu et al. 10.1016/j.quascirev.2021.107156
12. Air mass origin signals in δ 18O of tree-ring cellulose revealed by back-trajectory modeling at the monsoonal Tibetan plateau J. Wernicke et al. 10.1007/s00484-016-1292-y
13. Tree-ring δ18O inferred spring drought variability over the past 200 years in the Hengduan Mountains, Southwest China F. Zhao et al. 10.1016/j.palaeo.2018.12.020
14. Stable carbon isotopes from Torneträsk, northern Sweden provide a millennial length reconstruction of summer sunshine and its relationship to Arctic circulation N. Loader et al. 10.1016/j.quascirev.2012.11.014
15. Late Holocene relative humidity history on the southeastern Tibetan plateau inferred from a tree-ring δ 18 O record: Recent decrease and conditions during the last 1500 years J. Grießinger et al. 10.1016/j.quaint.2016.02.011
16. Central Himalayan tree-ring isotopes reveal increasing regional heterogeneity and enhancement in ice mass loss since the 1960s N. Singh et al. 10.5194/tc-15-95-2021
17. Global Evaluation of Proxy System Models for Stable Water Isotopes With Realistic Atmospheric Forcing A. Okazaki & K. Yoshimura 10.1029/2018JD029463
18. Multi-century humidity reconstructions from the southeastern Tibetan Plateau inferred from tree-ring δ18O J. Wernicke et al. 10.1016/j.gloplacha.2016.12.013
19. Assessing the past and future dynamics of the Asian summer monsoon: Insights from palaeomonsoon synthesis and CMIP6 data M. Shekhar et al. 10.1016/j.gecadv.2023.100004
20. Temporal evolution of the influence of atmospheric circulation on regional cloud cover as revealed by tree-ring δ18O in southwestern China W. Wang et al. 10.1016/j.gloplacha.2021.103690
21. Climatic aftermath of the 1815 Tambora eruption in China C. Gao et al. 10.1007/s13351-017-6091-9
22. Unstable relationships between tree ring δ18O and climate variables over southwestern China: possible impacts from increasing central Pacific SSTs W. An et al. 10.1007/s00704-018-2483-8
23. How is the El Niño–Southern Oscillation signal recorded by tree‐ring oxygen isotopes in southeastern China? C. Fang et al. 10.1002/joc.7601
24. Influence of the Indian Ocean Dipole on tree-ring δ18O of monsoonal Southeast Tibet P. Hochreuther et al. 10.1007/s10584-016-1663-8
25. Moisture source signals preserved in a 242-year tree-ring δ18O chronology in the western Himalaya M. Sano et al. 10.1016/j.gloplacha.2017.08.009
26. Recent strengthening of correlations between tree-ring δ13C and δ18O in mesic western China: Implications to climatic reconstruction and physiological responses X. Liu et al. 10.1016/j.gloplacha.2013.12.005
27. The spectrum of Asian Monsoon variability: A proxy system model approach to the hydroclimate scaling mismatch G. Loope et al. 10.1016/j.quascirev.2020.106362
28. A Dual Stable Isotope Approach Unravels Common Climate Signals and Species-Specific Responses to Environmental Change Stored in Multi-Century Tree-Ring Series from the Tibetan Plateau J. Grießinger et al. 10.3390/geosciences9040151
29. Drought variations in the southeastern Tibetan Plateau region since 1704 and their link to the Atlantic Multidecadal Oscillation W. Tang et al. 10.1016/j.palaeo.2023.111813
30. Catchment‐mediated atmospheric nitrogen deposition drives ecological change in two alpine lakes in SE Tibet Z. Hu et al. 10.1111/gcb.12435
31. Relative humidity history on the Batang–Litang Plateau of western China since 1755 reconstructed from tree-ring δ18O and δD W. An et al. 10.1007/s00382-013-1937-z
32. A shift in cloud cover over the southeastern Tibetan Plateau since 1600: evidence from regional tree-ring δ18O and its linkages to tropical oceans X. Liu et al. 10.1016/j.quascirev.2014.01.009
33. East Asian Summer Monsoon moisture sustains summer relative humidity in the southwestern Gobi Desert, China: evidence from δ18O of tree rings Q. Li et al. 10.1007/s00382-018-4515-6
34. Air moisture signals in a stable oxygen isotope chronology of dwarf shrubs from the central Tibetan Plateau J. Wernicke et al. 10.1093/aob/mcz030
35. Regional drought shifts (1710–2010) in East Central Asia and linkages with atmospheric circulation recorded in tree-ring δ18O G. Xu et al. 10.1007/s00382-018-4215-2
36. Relative humidity reconstruction for northwestern China’s Altay Mountains using tree-ring δ18O G. Xu et al. 10.1007/s11434-013-0055-y
37. No altitude‐dependent effects of climatic signals are recorded in Smith fir tree‐ring δ18O on the southeastern Tibetan Plateau, despite a shift in tree growth X. Zeng et al. 10.1111/bor.12053
38. Tree age, site and climate controls on tree ring cellulose δ18O: A case study on oak trees from south-western France I. Labuhn et al. 10.1016/j.dendro.2013.11.001
39. Can climate variations be inferred from tree-ring parameters and stable isotopes from Larix decidua? Juvenile effects, budmoth outbreaks, and divergence issue V. Daux et al. 10.1016/j.epsl.2011.07.003
40. High-resolution geochemical record for the last 1100 yr from Lake Toson, northeastern Tibetan Plateau, and its climatic implications Y. Ling et al. 10.1016/j.quaint.2017.03.067