77 citations as recorded by crossref.

1. Assessing forest vulnerability to climate warming using a process‐based model of tree growth: bad prospects for rear‐edges R. Sánchez‐Salguero et al. 10.1111/gcb.13541
2. The importance of input data quality and quantity in climate field reconstructions – results from the assimilation of various tree-ring collections J. Franke et al. 10.5194/cp-16-1061-2020
3. The climatic drivers of normalized difference vegetation index and tree‐ring‐based estimates of forest productivity are spatially coherent but temporally decoupled in Northern Hemispheric forests K. Seftigen et al. 10.1111/geb.12802
4. Northeastern North America as a potential refugium for boreal forests in a warming climate L. D’Orangeville et al. 10.1126/science.aaf4951
5. Possible Increase of Vegetation Exposure to Spring Frost under Climate Change in Switzerland O. Lhotka & S. Brönnimann 10.3390/atmos11040391
6. Decadal–centennial hydroclimate variability over eastern China during the last millennium: Results from the product of Paleo Hydrodynamics Data Assimilation Y. Peng 10.1016/j.aosl.2021.100038
7. Testing the performance of dendroclimatic process-based models at global scale with the PAGES2k tree-ring width database J. Rezsöhazy et al. 10.1007/s00382-021-05789-7
8. New tree-ring data from Canadian boreal and hemi-boreal forests provide insight for improving the climate sensitivity of terrestrial biosphere models A. Mirabel et al. 10.1016/j.scitotenv.2022.158062
9. Process representation of conifer tree-ring growth is improved by incorporation of climate memory effects X. ZENG et al. 10.1016/j.agrformet.2022.109196
10. Climate field reconstruction uncertainty arising from multivariate and nonlinear properties of predictors M. Evans et al. 10.1002/2014GL062063
11. Application and evaluation of the dendroclimatic process-based model MAIDEN during the last century in Canada and Europe J. Rezsöhazy et al. 10.5194/cp-16-1043-2020
12. Challenges and perspectives for large‐scale temperature reconstructions of the past two millennia B. Christiansen & F. Ljungqvist 10.1002/2016RG000521
13. Tree growth decline as a response to projected climate change in the 21st century in Mediterranean mountain forests of Chile V. Matskovsky et al. 10.1016/j.gloplacha.2020.103406
14. A triple tree-ring constraint for tree growth and physiology in a global land surface model J. Barichivich et al. 10.5194/bg-18-3781-2021
15. rwl_read: A MATLAB program to identify and correct formatting errors in tree-ring measurement files Y. Liu 10.1016/j.softx.2022.101285
16. An Artificial Neural Networks‐Based Tree Ring Width Proxy System Model for Paleoclimate Data Assimilation M. Fang & X. Li 10.1029/2018MS001525
17. Atmospheric dynamics drive most interannual U.S. droughts over the last millennium M. Erb et al. 10.1126/sciadv.aay7268
18. Last Millennium ENSO Diversity and North American Teleconnections: New Insights From Paleoclimate Data Assimilation X. Luo et al. 10.1029/2021PA004283
19. Two types of North American droughts related to different atmospheric circulation patterns A. Burgdorf et al. 10.5194/cp-15-2053-2019
20. Seasonal Growth of Pine Tree Rings: Comparison of Direct Observations and Simulation E. Babushkina et al. 10.3390/f13121978
21. Predicting spatiotemporal variability in radial tree growth at the continental scale with machine learning P. Bodesheim et al. 10.1017/eds.2022.8
22. Insights into the BRT (Boosted Regression Trees) Method in the Study of the Climate-Growth Relationship of Masson Pine in Subtropical China H. Gu et al. 10.3390/f10030228
23. Should artificial neural networks replace linear models in tree ring based climate reconstructions? J. Jevšenak & T. Levanič 10.1016/j.dendro.2016.08.002
24. Non-linear modelling reveals a predominant moisture limit on juniper growth across the southern Tibetan Plateau H. Jia et al. 10.1093/aob/mcac065
25. Evidence of advancing spring xylem phenology in Chinese forests under global warming H. Xue et al. 10.1007/s11430-022-1149-x
26. A tree-ring perspective on the terrestrial carbon cycle F. Babst et al. 10.1007/s00442-014-3031-6
27. Climate response of oak (Quercus spp.), an evidence of a bioclimatic boundary induced by the Carpathians C. Nechita et al. 10.1016/j.scitotenv.2017.05.118
28. An overview of tree-ring width records across the Northern Hemisphere S. St. George 10.1016/j.quascirev.2014.04.029
29. Tropical Pacific Modulation of the Asian Summer Monsoon Over the Last Millennium in Paleoclimate Data Assimilation Reconstructions J. Hu et al. 10.1029/2023JD039207
30. Different Radial Growth Responses to Climate Change of Three Dominant Conifer Species in Temperate Forest, Northeastern China H. Wang et al. 10.3389/ffgc.2021.820800
31. Climate change detection and attribution using observed and simulated tree-ring width J. Franke et al. 10.5194/cp-18-2583-2022
32. A reconstruction of global hydroclimate and dynamical variables over the Common Era N. Steiger et al. 10.1038/sdata.2018.86
33. DOCU-CLIM: A global documentary climate dataset for climate reconstructions A. Burgdorf et al. 10.1038/s41597-023-02303-y
34. The summer standardized precipitation evapotranspiration index (SPEI) dataset for six European regions over the past millennium reconstructed by tree-ring chronologies L. Zhang et al. 10.1080/20964471.2023.2247864
35. Correlation and causation in tree‐ring‐based reconstruction of paleohydrology in cold semiarid regions A. Elshorbagy et al. 10.1002/2016WR018985
36. A monthly global paleo-reanalysis of the atmosphere from 1600 to 2005 for studying past climatic variations J. Franke et al. 10.1038/sdata.2017.76
37. Last Millennium Reanalysis with an expanded proxy database and seasonal proxy modeling R. Tardif et al. 10.5194/cp-15-1251-2019
38. Was the Little Ice Age more or less El Niño-like than the Medieval Climate Anomaly? Evidence from hydrological and temperature proxy data L. Henke et al. 10.5194/cp-13-267-2017
39. Increased growth of Qinghai spruce in northwestern China during the recent warming hiatus L. Gao et al. 10.1016/j.agrformet.2018.05.025
40. The International Tree‐Ring Data Bank (ITRDB) revisited: Data availability and global ecological representativity S. Zhao et al. 10.1111/jbi.13488
41. Paleoclimate data assimilation: Its motivation, progress and prospects M. Fang & X. Li 10.1007/s11430-015-5432-6
42. Climate Warming Alters Age-Dependent Growth Sensitivity to Temperature in Eurasian Alpine Treelines R. Sanchez-Salguero et al. 10.3390/f9110688
43. Modeled Tracheidograms Disclose Drought Influence on Pinus sylvestris Tree-Rings Structure From Siberian Forest-Steppe M. Popkova et al. 10.3389/fpls.2018.01144
44. An interpreted language implementation of the Vaganov–Shashkin tree-ring proxy system model K. Anchukaitis et al. 10.1016/j.dendro.2020.125677
45. Spatial patterns of precipitation-induced moisture availability and their effects on the divergence of conifer stem growth in the western and eastern parts of China’s semi-arid region X. Zeng et al. 10.1016/j.foreco.2019.117524
46. Species-specific climate–growth interactions determine tree species dynamics in mixed Central European mountain forests J. Kašpar et al. 10.1088/1748-9326/abd8fb
47. Dendrobox – An interactive exploration tool for the International Tree Ring Data Bank C. Zang 10.1016/j.dendro.2014.10.002
48. Assimilation of pseudo-tree-ring-width observations into an atmospheric general circulation model W. Acevedo et al. 10.5194/cp-13-545-2017
49. Forward Modeling Reveals Multidecadal Trends in Cambial Kinetics and Phenology at Treeline J. Tumajer et al. 10.3389/fpls.2021.613643
50. Disentangling the multi-faceted growth patterns of primary Picea abies forests in the Carpathian arc J. Björklund et al. 10.1016/j.agrformet.2019.03.002
51. Response of Larix chinensis Radial Growth to Climatic Factors Using the Process-Based Vaganov–Shashkin-Lite Model at Mt. Taibai, China S. Li et al. 10.3390/f13081252
52. Process-Based Modeling of Phenology and Radial Growth in Pinus tabuliformis in Response to Climate Factors over a Cold and Semi-Arid Region Z. Man et al. 10.3390/plants13070980
53. How can the parameterization of a process-based model help us understand real tree-ring growth? I. Tychkov et al. 10.1007/s00468-018-1780-2
54. Linkage between growth phenology and climate-growth responses along landscape gradients in boreal forests J. Tumajer et al. 10.1016/j.scitotenv.2023.167153
55. Assimilating an expanded tree ring dataset to reconstruct the millennial air temperature fields for the Northern Hemisphere M. Fang et al. 10.1002/joc.7528
56. Daily climate data reveal stronger climate-growth relationships for an extended European tree-ring network J. Jevšenak 10.1016/j.quascirev.2019.105868
57. Drought explains variation in the radial growth of white spruce in western Canada L. Chen et al. 10.1016/j.agrformet.2016.11.012
58. An additional step toward comprehensive paleoclimate reanalyses H. Goosse 10.1002/2016MS000739
59. Comparing proxy and model estimates of hydroclimate variability and change over the Common Era 10.5194/cp-13-1851-2017
60. Forward modeling of tree-ring width improves simulation of forest growth responses to drought M. Mina et al. 10.1016/j.agrformet.2016.02.005
61. Converging Climate Sensitivities of European Forests Between Observed Radial Tree Growth and Vegetation Models Z. Zhang et al. 10.1007/s10021-017-0157-5
62. Tunneling-induced groundwater depletion limits long-term growth dynamics of forest trees H. Behzad et al. 10.1016/j.scitotenv.2021.152375
63. Resist, recover or both? Growth plasticity in response to drought is geographically structured and linked to intraspecific variability in Pinus pinaster R. Sánchez‐Salguero et al. 10.1111/jbi.13202
64. Beyond meteorological data: Modelling tree growth with ERA5-Land M. Schönauer et al. 10.1016/j.agrformet.2025.110679
65. Temporal changes in climatic limitation of tree-growth at upper treeline forests: Contrasted responses along the west-to-east humidity gradient in Northern Patagonia A. Lavergne et al. 10.1016/j.dendro.2015.09.001
66. Towards the assimilation of tree-ring-width records using ensemble Kalman filtering techniques W. Acevedo et al. 10.1007/s00382-015-2683-1
67. Impact of Disturbance Signatures on Tree Ring Width and Blue Intensity Chronology Structure and Climatic Signals in Carpathian Norway Spruce Y. Jiang et al. 10.2139/ssrn.4089131
68. Increasing moisture limitation of Norway spruce in Central Europe revealed by forward modelling of tree growth in tree-ring network J. Tumajer et al. 10.1016/j.agrformet.2017.07.015
69. Growth-limiting factors and climate response variability in Norway spruce (Picea abies L.) along an elevation and precipitation gradients in Slovenia J. Jevšenak et al. 10.1007/s00484-020-02033-5
70. ModE-RA: a global monthly paleo-reanalysis of the modern era 1421 to 2008 V. Valler et al. 10.1038/s41597-023-02733-8
71. Impact of disturbance signatures on tree-ring width and blue intensity chronology structure and climatic signals in Carpathian Norway spruce Y. Jiang et al. 10.1016/j.agrformet.2022.109236
72. Contrasting growth responses in Himalayan trees to future climate R. Dhyani et al. 10.1016/j.scitotenv.2025.179700
73. 古气候数据同化<bold>: </bold>缘起<bold>、</bold>进展与展望 苗. 方 & 新. 李 10.1360/N072015-00432
74. When tree rings go global: Challenges and opportunities for retro- and prospective insight F. Babst et al. 10.1016/j.quascirev.2018.07.009
75. Climate sensitivity of seasonal radial growth in young stands of Mexican conifers M. Pompa-García et al. 10.1007/s00484-022-02312-3
76. The Historical Development of Large‐Scale Paleoclimate Field Reconstructions Over the Common Era J. Smerdon et al. 10.1029/2022RG000782
77. Probabilistic reconstructions of local temperature and soil moisture from tree-ring data with potentially time-varying climatic response S. Tolwinski-Ward et al. 10.1007/s00382-014-2139-z