All Stories

  1. Anomalously depleted δ2H signatures of tropical cyclone precipitation recorded in tree-ring lignin methoxy groups
  2. Competition and vapor pressure deficit drive the mortality of Qinghai spruce (Picea crassifolia) in the eastern Qilian mountains
  3. Exacerbated Variability and Extremes in Streamflow Across Half of China From 1961 to 2018
  4. Enhanced moisture-sensitivity increased the growth variability of Picea purpurea in the northeastern Tibetan Plateau
  5. A Millennium of ENSO Influence on Jet Stream Driven Summer Climate Extremes
  6. Climate suitability for the moisture-sensitive conifer species may not be universally declining in a warming world
  7. Jet stream controls on European climate and agriculture since 1300 ce
  8. Management can mitigate drought legacy effects on the growth of a moisture-sensitive conifer tree species
  9. A Seasonally Varying Tree Physiological Response to Environmental Conditions: Results From Semi‐Arid China
  10. Intra-annual tree-ring δ18O and δ13C reveal a trade-off between isotopic source and humidity in moist environments
  11. 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
  12. Jet stream position explains regional anomalies in European beech forest productivity and tree growth
  13. 800 years of summer European-North Atlantic jet stream variability and its impact on climate extremes and human systems
  14. Strongly Active Responses of Pinus Tabuliformis and Sophora Viciifolia to Co2 Enrichment and Drought Revealed by Tree Ring Isotopes on the Central China's Loess Plateau
  15. Europe-Atlantic jet caused dipole mode of European climate and increased climatic extremes
  16. Jet stream position connected to atmospheric blocking drives regional anomalies in European forest productivity
  17. Discrepancy in Growth Resilience to Drought Among Different Stand-Aged Forests Declines Going from a Semi-Humid Region to an Arid Region
  18. Seasonal divergence between soil water availability and atmospheric moisture recorded in intra-annual tree-ring δ18O extremes
  19. Young trees have the potential to improve climate reconstruction
  20. Similar potential of foliar δ13C and silicon levels for inferring local climate information in the Tibetan Plateau region
  21. Tibetan Plateau temperature variability in the past 1000 years
  22. CO 2 fertilization confounds tree ring records of regional hydroclimate at northeastern Qinghai‐Tibetan Plateau
  23. Leaf Age Compared to Tree Age Plays a Dominant Role in Leaf δ13C and δ15N of Qinghai Spruce (Picea crassifolia Kom.)
  24. Disentangling Contributions of CO2 Concentration and Climate to Changes in Intrinsic Water-Use Efficiency in the Arid Boreal Forest in China’s Altay Mountains
  25. 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
  26. Increased mercury pollution revealed by tree rings from the China’s Tianshan Mountains
  27. Unstable relationships between tree ring δ18O and climate variables over southwestern China: possible impacts from increasing central Pacific SSTs
  28. Spatiotemporal variability of drought in the northern part of northeast China
  29. Drought changes in Central Asia and Xinjiang, China
  30. 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
  31. Anthropogenic-management could mitigate declines in growth and survival of Qinghai spruce (Picea crassifolia) in the east Qilian Mountains, northeast Tibetan Plateau
  32. OUP accepted manuscript
  33. 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
  34. Climate signals in tree-ring δ18 O and δ13 C from southeastern Tibet: insights from observations and forward modelling of intra- to interdecadal variability
  35. Reconstructed Inter-Annual Variation in September–October Precipitation for the Upper Reaches of the Heihe River and Its Implications for Regional Drought Conditions
  36. Tree ring δ18 O reveals no long-term change of atmospheric water demand since 1800 in the northern Great Hinggan Mountains, China
  37. Reconstructed annual mean temperatures for the northeastern margin of the Tibetan Plateau: associations with the East Asian monsoons and volcanic events
  38. Seasonal incursion of Indian Monsoon humidity and precipitation into the southeastern Qinghai–Tibetan Plateau inferred from tree ring δO18 values with intra-seasonal resolution
  39. Temperature signal instability of tree-ring δ 13 C chronology in the northeastern Qinghai–Tibetan Plateau
  40. Alpine timberline population dynamics under climate change, NE Tibetan Plateau
  41. Qinghai spruce growth–climate response between lower and upper elevation gradient limits
  42. Differential response of Qilian juniper radial growth to climate variations in the middle of Qilian Mountains and the northeastern Qaidam Basin
  43. Tree ringδ18O's indication of a shift to a wetter climate since the 1880s in the western Tianshan Mountains of northwestern China
  44. 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
  45. Elevation-dependent variations of tree growth and intrinsic water-use efficiency in Schrenk spruce (Picea schrenkiana) in the western Tianshan Mountains, China
  46. Pooled versus separate tree-ring δD measurements, and implications for reconstruction of the Arctic Oscillation in northwestern China
  47. Tree growth and intrinsic water-use efficiency of inland riparian forests in northwestern China: evaluation via  13C and  18O analysis of tree rings
  48. A shift in cloud cover over the southeastern Tibetan Plateau since 1600: evidence from regional tree-ring δ18O and its linkages to tropical oceans
  49. 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
  50. Recent strengthening of correlations between tree-ring δ13C and δ18O in mesic western China: Implications to climatic reconstruction and physiological responses
  51. Relative humidity reconstruction for northwestern China’s Altay Mountains using tree-ring δ18O
  52. Tree-ring δ18 O evidence for the drought history of eastern Tianshan Mountains, northwest China since 1700 AD
  53. 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
  54. Relative humidity history on the Batang–Litang Plateau of western China since 1755 reconstructed from tree-ring δ18O and δD
  55. 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
  56. Moisture variations over the past millennium characterized by Qaidam Basin tree-ring δ 18O
  57. A 400-year tree-ring δ18O chronology for the southeastern Tibetan Plateau: Implications for inferring variations of the regional hydroclimate
  58. Climate warming and increasing atmospheric CO2 have contributed to increased intrinsic water-use efficiency on the northeastern Tibetan Plateau since 1850
  59. Age-dependent tree-ring growth responses of Schrenk spruce (Picea schrenkiana) to climate—A case study in the Tianshan Mountain, China
  60. Increased intrinsic water-use efficiency during a period with persistent decreased tree radial growth in northwestern China: Causes and implications
  61. Specific climatic signals recorded in earlywood and latewood δ18O of tree rings in southwestern China
  62. 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
  63. Tree ring stable isotope recorded the monsoon decrease
  64. Summer temperature variations recorded in tree-ring δ13C values on the northeastern Tibetan Plateau
  65. Climatic significance of tree-ring δ18O in the Qilian Mountains, northwestern China and its relationship to atmospheric circulation patterns