59 citations as recorded by crossref.

1. The triple oxygen isotope composition of phytoliths as a proxy of continental atmospheric humidity: insights from climate chamber and climate transect calibrations A. Alexandre et al. 10.5194/bg-15-3223-2018
2. Stable oxygen isotopes in juniper and oak tree rings from northern Iran as indicators for site-specific and season-specific moisture variations Z. Foroozan et al. 10.1016/j.dendro.2015.08.003
3. 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
4. Lake diatom response to climate change and sedimentary events on the southeastern Tibetan Plateau during the last millennium M. Liao et al. 10.1016/j.quascirev.2020.106409
5. 501 Years of Spring Precipitation History for the Semi-Arid Northern Iran Derived from Tree-Ring δ18O Data Z. Foroozan et al. 10.3390/atmos11090889
6. 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
7. Modelling tree ring cellulose δ18O variations in two temperature-sensitive tree species from North and South America A. Lavergne et al. 10.5194/cp-13-1515-2017
8. Anthropogenic forcing has impacted precipitation variability in the North China Monsoon Marginal Region X. Zhao et al. 10.1016/j.palaeo.2025.113180
9. Treeline composition and biodiversity change on the southeastern Tibetan Plateau during the past millennium, inferred from a high-resolution alpine pollen record K. Li et al. 10.1016/j.quascirev.2018.12.029
10. Oxygen isotope ratios of subalpine conifers in Jirisan National Park, Korea and their dendroclimatic potential J. Seo et al. 10.1016/j.dendro.2019.125626
11. Oxygen isotope enrichment in rice (Oryza sativa L.) grain organic matter captures signature of relative humidity R. Kaushal & P. Ghosh 10.1016/j.plantsci.2018.05.022
12. 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
13. Climate signals in tree‐ring δ18O and δ13C from southeastern Tibet: insights from observations and forward modelling of intra‐ to interdecadal variability X. Zeng et al. 10.1111/nph.14750
14. 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
15. Last 1100 yr of precipitation variability in western central Asia as revealed by tree-ring data from the Pamir-Alay M. Opała-Owczarek & T. Niedźwiedź 10.1017/qua.2018.21
16. ENSO variability reflected in precipitation oxygen isotopes across the Asian Summer Monsoon region Z. Cai et al. 10.1016/j.epsl.2017.06.035
17. 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
18. May–June drought reconstruction over the past 821 years on the south-central Tibetan Plateau derived from tree-ring width series M. He et al. 10.1016/j.dendro.2017.12.006
19. Multi-centennial reconstruction of drought events in South-Western Iran using tree rings of Mediterranean cypress (Cupressus sempervirens L.) M. Arsalani et al. 10.1016/j.palaeo.2021.110296
20. 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
21. Negligible local-factor influences on tree ring cellulose δ¹⁸O of Qilian juniper in the Animaqing Mountains of the eastern Tibetan Plateau C. Xu et al. 10.1080/16000889.2017.1391663
22. Recent decline of high altitude coniferous growth due to thermo-hydraulic constrains: evidence from the Miyaluo Forest Reserve, Western Sichuan Plateau of China M. Keyimu et al. 10.1016/j.dendro.2020.125751
23. Glaciations and palaeoclimate of the last millennium in the Drongtso Lungpa Co Valley, southeastern Tibetan Plateau, based on cosmogenic 10Be exposure dating and glacier modelling Z. Jiang et al. 10.1016/j.jseaes.2023.105777
24. Proglacial lake response to Late-Holocene glacial fluctuations in Southeast Tibet F. Lemot et al. 10.1016/j.gloplacha.2023.104347
25. Drought increased the response sensitivity of tree-ring δ18O for Qinghai spruce to climate change at different elevations in the eastern Tibetan Plateau Y. Qin et al. 10.1016/j.quaint.2025.109827
26. High resolution monsoon precipitation changes on southeastern Tibetan Plateau over the past 2300 years L. Tan et al. 10.1016/j.quascirev.2018.07.021
27. Improved spectral comparisons of paleoclimate models and observations via proxy system modeling: Implications for multi-decadal variability S. Dee et al. 10.1016/j.epsl.2017.07.036
28. 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
29. Weakening of the Summer Monsoon Over the Past 150 Years Shown by a Tree‐Ring Record From Shandong, Eastern China, and the Potential Role of North Atlantic Climate Q. Chen et al. 10.1029/2022PA004495
30. Hydrological Extremes in the Upper Yangtze River Over the Past 700 yr Inferred From a Tree Ring δ18O Record W. An et al. 10.1029/2021JD036109
31. Tree-Ring Oxygen Isotope Variations in Subalpine Firs from the Western Himalaya Capture Spring Season Temperature Signals B. Chinthala et al. 10.3390/f13030437
32. 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
33. 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
34. Warming-induced unprecedented high-elevation forest growth over the monsoonal Tibetan Plateau C. Shi et al. 10.1088/1748-9326/ab7b9b
35. Bi-decadal climate reconstruction derived from a 1200-year long pollen record from the NE Qinghai-Tibet Plateau and its implications for discussion of the late Holocene environmental dynamics C. Müller 10.1016/j.quaint.2017.05.058
36. Stable Oxygen and Carbon Isotopic Composition of Rice (Oryza sativa L.) Grains as Recorder of Relative Humidity R. Kaushal & P. Ghosh 10.1002/2017JG004245
37. Hydroclimatic seasonality recorded by tree ring δ18O signature across a Himalayan altitudinal transect C. Brunello et al. 10.1016/j.epsl.2019.04.030
38. Millennium-Long Tree-Ring Chronology Reveals Megadroughts on the Southeastern Tibetan Plateau C. Nie et al. 10.3959/1536-1098-73.1.1
39. Influence of the Indian Ocean Dipole on tree-ring δ18O of monsoonal Southeast Tibet P. Hochreuther et al. 10.1007/s10584-016-1663-8
40. Irrawaddy River experienced more frequent hydrological drought events with global warming: Evidence from a 400-year tree ring oxygen isotope record Y. Zhao et al. 10.1016/j.catena.2023.107455
41. 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
42. Sampling strategy and climatic implication of tree-ring cellulose oxygen isotopes of Hippophae tibetana and Abies georgei on the southeastern Tibetan Plateau C. Xu et al. 10.1007/s00484-017-1365-6
43. A 406-year non-growing-season precipitation reconstruction in the southeastern Tibetan Plateau M. Keyimu et al. 10.5194/cp-17-2381-2021
44. 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
45. Enhanced Variability and Declining Trend of Soil Moisture Since the 1880s on the Southeastern Tibetan Plateau L. Wang et al. 10.1029/2022WR033953
46. Tree rings reveal hydroclimatic fingerprints of the Pacific Decadal Oscillation on the Tibetan Plateau L. Lyu et al. 10.1007/s00382-019-04629-z
47. Asian summer monsoon variability, global teleconnections, and dynamics during the last 1,000 years M. Shekhar et al. 10.1016/j.earscirev.2022.104041
48. Evaluation of Different Pooling Methods to Establish a Multi-Century δ18O Chronology for Paleoclimate Reconstruction Z. Foroozan et al. 10.3390/geosciences9060270
49. Decreasing monsoon precipitation in southwest China during the last 240 years associated with the warming of tropical ocean L. Tan et al. 10.1007/s00382-016-3171-y
50. The relationship between climate and the intra-annual oxygen isotope patterns from pine trees: a case study along an elevation gradient on Corsica, France S. Szymczak et al. 10.1007/s13595-019-0860-9
51. Unenriched xylem water contribution during cellulose synthesis influenced by atmospheric demand governs the intra‐annual tree‐ring δ18O signature E. Martínez‐Sancho et al. 10.1111/nph.19278
52. Temperature variations since 1750 CE inferred from an alpine lake in the southeastern margin of the Tibetan Plateau J. Li et al. 10.1016/j.quaint.2016.12.016
53. 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
54. Global Evaluation of Proxy System Models for Stable Water Isotopes With Realistic Atmospheric Forcing A. Okazaki & K. Yoshimura 10.1029/2018JD029463
55. Tree ring oxygen isotope in Asia C. Xu et al. 10.1016/j.gloplacha.2023.104348
56. Tree-rings stable isotope (δ18O and δ2H) based 368 years long term precipitation reconstruction of South Eastern Kashmir Himalaya U. Pandey et al. 10.1016/j.scitotenv.2023.164640
57. Decreasing Indian summer monsoon on the northern Indian sub-continent during the last 180 years: evidence from five tree-ring cellulose oxygen isotope chronologies C. Xu et al. 10.5194/cp-14-653-2018
58. Variability of summer humidity during the past 800 years on the eastern Tibetan Plateau inferred from δ18O of tree-ring cellulose J. Wernicke et al. 10.5194/cp-11-327-2015
59. A modelling approach to reconstruct Little Ice Age climate from remote-sensing glacier observations in southeastern Tibet E. Huintjes et al. 10.3189/2016AoG71A025