All Stories

  1. Intra-annual tree-ring δ18O and δ13C reveal a trade-off between isotopic source and humidity in moist environments
  2. Strongly Active Responses of Pinus tabuliformis Carr. and Sophora viciifolia Hance to CO2 Enrichment and Drought Revealed by Tree-Ring Isotopes on the Central China Loess Plateau
  3. Jet stream position explains regional anomalies in European beech forest productivity and tree growth
  4. 800 years of summer European-North Atlantic jet stream variability and its impact on climate extremes and human systems
  5. Europe-Atlantic jet caused dipole mode of European climate and increased climatic extremes
  6. Jet stream position connected to atmospheric blocking drives regional anomalies in European forest productivity
  7. Seasonal divergence between soil water availability and atmospheric moisture recorded in intra-annual tree-ring δ18O extremes
  8. Young trees have the potential to improve climate reconstruction
  9. Similar potential of foliar δ13C and silicon levels for inferring local climate information in the Tibetan Plateau region
  10. Tibetan Plateau temperature variability in the past 1000 years
  11. CO 2 fertilization confounds tree ring records of regional hydroclimate at northeastern Qinghai‐Tibetan Plateau
  12. Disentangling Contributions of CO2 Concentration and Climate to Changes in Intrinsic Water-Use Efficiency in the Arid Boreal Forest in China’s Altay Mountains
  13. Application and verification of simultaneous determination of cellulose δ13C and δ18O in Picea shrenkiana tree rings from northwestern China using the high-temperature pyrolysis method
  14. Increased mercury pollution revealed by tree rings from the China’s Tianshan Mountains
  15. Unstable relationships between tree ring δ18O and climate variables over southwestern China: possible impacts from increasing central Pacific SSTs
  16. Spatiotemporal variability of drought in the northern part of northeast China
  17. Drought changes in Central Asia and Xinjiang, China
  18. Age-dependent impacts of climate change and intrinsic water-use efficiency on the growth of Schrenk spruce (Picea schrenkiana) in the western Tianshan Mountains, China
  19. Anthropogenic-management could mitigate declines in growth and survival of Qinghai spruce (Picea crassifolia) in the east Qilian Mountains, northeast Tibetan Plateau
  20. OUP accepted manuscript
  21. Species-specific tree growth and intrinsic water-use efficiency of Dahurian larch ( Larix gmelinii ) and Mongolian pine ( Pinus sylvestris var. mongolica ) growing in a boreal permafrost region of the Greater Hinggan Mountains, Northeastern China
  22. Climate signals in tree-ring δ18 O and δ13 C from southeastern Tibet: insights from observations and forward modelling of intra- to interdecadal variability
  23. Reconstructed Inter-Annual Variation in September–October Precipitation for the Upper Reaches of the Heihe River and Its Implications for Regional Drought Conditions
  24. Tree ring δ18 O reveals no long-term change of atmospheric water demand since 1800 in the northern Great Hinggan Mountains, China
  25. Reconstructed annual mean temperatures for the northeastern margin of the Tibetan Plateau: associations with the East Asian monsoons and volcanic events
  26. Seasonal incursion of Indian Monsoon humidity and precipitation into the southeastern Qinghai–Tibetan Plateau inferred from tree ring δO18 values with intra-seasonal resolution
  27. Temperature signal instability of tree-ring δ 13 C chronology in the northeastern Qinghai–Tibetan Plateau
  28. Alpine timberline population dynamics under climate change, NE Tibetan Plateau
  29. Qinghai spruce growth–climate response between lower and upper elevation gradient limits
  30. Differential response of Qilian juniper radial growth to climate variations in the middle of Qilian Mountains and the northeastern Qaidam Basin
  31. Tree ringδ18O's indication of a shift to a wetter climate since the 1880s in the western Tianshan Mountains of northwestern China
  32. Long-term variation of tree growth and intrinsic water-use efficiency in Schrenk spruce with increasing CO2 concentration and climate warming in the western Tianshan Mountains, China
  33. Elevation-dependent variations of tree growth and intrinsic water-use efficiency in Schrenk spruce (Picea schrenkiana) in the western Tianshan Mountains, China
  34. Pooled versus separate tree-ring δD measurements, and implications for reconstruction of the Arctic Oscillation in northwestern China
  35. Tree growth and intrinsic water-use efficiency of inland riparian forests in northwestern China: evaluation via  13C and  18O analysis of tree rings
  36. A shift in cloud cover over the southeastern Tibetan Plateau since 1600: evidence from regional tree-ring δ18O and its linkages to tropical oceans
  37. Tree-ring growth recovers, but δ13C and δ15N do not change, after the removal of point-source air pollution: a case study for poplar (Populus cathayana) in northwestern China
  38. Recent strengthening of correlations between tree-ring δ13C and δ18O in mesic western China: Implications to climatic reconstruction and physiological responses
  39. Relative humidity reconstruction for northwestern China’s Altay Mountains using tree-ring δ18O
  40. Tree-ring δ18 O evidence for the drought history of eastern Tianshan Mountains, northwest China since 1700 AD
  41. 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
  42. Relative humidity history on the Batang–Litang Plateau of western China since 1755 reconstructed from tree-ring δ18O and δD
  43. Drought history inferred from tree ring δ 13C and δ 18O in the central Tianshan Mountains of China and linkage with the North Atlantic Oscillation
  44. Moisture variations over the past millennium characterized by Qaidam Basin tree-ring δ 18O
  45. A 400-year tree-ring δ18O chronology for the southeastern Tibetan Plateau: Implications for inferring variations of the regional hydroclimate
  46. Climate warming and increasing atmospheric CO2 have contributed to increased intrinsic water-use efficiency on the northeastern Tibetan Plateau since 1850
  47. Age-dependent tree-ring growth responses of Schrenk spruce (Picea schrenkiana) to climate—A case study in the Tianshan Mountain, China
  48. Increased intrinsic water-use efficiency during a period with persistent decreased tree radial growth in northwestern China: Causes and implications
  49. Specific climatic signals recorded in earlywood and latewood δ18O of tree rings in southwestern China
  50. A 200 year temperature record from tree ringδ13C at the Qaidam Basin of the Tibetan Plateau after identifying the optimum method to correct for changing atmospheric CO2andδ13C
  51. Tree ring stable isotope recorded the monsoon decrease
  52. Summer temperature variations recorded in tree-ring δ13C values on the northeastern Tibetan Plateau
  53. Climatic significance of tree-ring δ18O in the Qilian Mountains, northwestern China and its relationship to atmospheric circulation patterns