33 citations as recorded by crossref.

1. Bayesian multiproxy temperature reconstruction with black spruce ring widths and stable isotopes from the northern Quebec taiga F. Gennaretti et al. 10.1007/s00382-017-3565-5
2. Tropical volcanoes synchronize eastern Canada with Northern Hemisphere millennial temperature variability F. Wang et al. 10.1038/s41467-022-32682-6
3. Major postglacial summer temperature changes in the central coniferous boreal forest of Quebec (Canada) inferred using chironomid assemblages L. Bajolle et al. 10.1002/jqs.3022
4. Recent human-induced atmospheric drying across Europe unprecedented in the last 400 years K. Treydte et al. 10.1038/s41561-023-01335-8
5. Methodological constrains of tree-ring stable isotope chronologies T. Arosio et al. 10.1016/j.quascirev.2024.108861
6. Oxygen Isotopes in Tree Rings from Greenland: A New Proxy of NAO C. Xu et al. 10.3390/atmos12010039
7. Relevance of using whole-ring stable isotopes of black spruce trees in the perspective of climate reconstruction C. Alvarez et al. 10.1016/j.dendro.2018.05.004
8. Tree-ring cellulose δ18O records similar large-scale climate influences as precipitation δ18O in the Northwest Territories of Canada R. Field et al. 10.1007/s00382-021-05932-4
9. Tree-ring stable isotopes for regional discharge reconstruction in eastern Labrador and teleconnection with the Arctic Oscillation L. Dinis et al. 10.1007/s00382-019-04731-2
10. Forced changes in the Pacific Walker circulation over the past millennium G. Falster et al. 10.1038/s41586-023-06447-0
11. Last millennium Northern Hemisphere summer temperatures from tree rings: Part II, spatially resolved reconstructions K. Anchukaitis et al. 10.1016/j.quascirev.2017.02.020
12. Reconstructing past hydrology of eastern Canadian boreal catchments using clastic varved sediments and hydro-climatic modelling: 160 years of fluvial inflows A. Gagnon-Poiré et al. 10.5194/cp-17-653-2021
13. A 7.5 ka chronology of stable carbon isotopes from tree rings with implications for their use in palaeo-cloud reconstruction S. Helama et al. 10.1016/j.gloplacha.2018.08.002
14. Recent atmospheric drying in Siberia is not unprecedented over the last 1,500 years O. Churakova Sidorova et al. 10.1038/s41598-020-71656-w
15. Spring arctic oscillation as a trigger of summer drought in Siberian subarctic over the past 1494 years O. Churakova Sidorova et al. 10.1038/s41598-021-97911-2
16. 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
17. Tree-ring δ18O from an Alpine catchment reveals changes in glacier stream water inputs between 1980 and 2010 G. Leonelli et al. 10.1080/15230430.2019.1623607
18. A new snow module improves predictions of the isotope-enabled MAIDENiso forest growth model I. Hermoso de Mendoza et al. 10.5194/gmd-15-1931-2022
19. Evaluation of the non-climatic (age-related) trends of stable oxygen and carbon isotopes in Swiss stone pine (Pinus cembra L.) tree rings from the Eastern Carpathians, Romania Z. Kern et al. 10.1016/j.dendro.2023.126061
20. Spatial variation of hydroclimate in north-eastern North America during the last millennium H. Mackay et al. 10.1016/j.quascirev.2021.106813
21. Spatial and temporal dimensions of fire activity in the fire‐prone eastern Canadian taiga S. Erni et al. 10.1111/gcb.13461
22. The global potential of log-driven trees for reconstructing forest ecosystems dynamics J. Labrecque-Foy & M. Montoro Girona 10.3389/fevo.2023.1232543
23. Recent peat and carbon accumulation following the Little Ice Age in northwestern Québec, Canada S. Piilo et al. 10.1088/1748-9326/ab11ec
24. 400 Years of summer hydroclimate from stable isotopes in Iberian trees L. Andreu-Hayles et al. 10.1007/s00382-016-3332-z
25. Tree-ring δ18Ocellulose variations in two Nothofagus species record large-scaleclimatic signals in the South American sector of the Southern Ocean P. Soto-Rogel et al. 10.1016/j.palaeo.2023.111474
26. Evaluation of Different Pooling Methods to Establish a Multi-Century δ18O Chronology for Paleoclimate Reconstruction Z. Foroozan et al. 10.3390/geosciences9060270
27. Response strategies of boreal spruce trees to anthropogenic changes in air quality and rising pCO2 M. Savard et al. 10.1016/j.envpol.2020.114209
28. Climate impacts on tree-ring stable isotopes across the Northern Hemispheric boreal zone O. Churakova (Sidorova) et al. 10.1016/j.scitotenv.2023.161644
29. French summer droughts since 1326 CE: a reconstruction based on tree ring cellulose <i>δ</i><sup>18</sup>O I. Labuhn et al. 10.5194/cp-12-1101-2016
30. Hydroclimate variability in the Tropical Andes recorded by δ18O isotopes from a new network of Polylepis tarapacana tree-rings C. Álvarez et al. 10.1016/j.gloplacha.2024.104503
31. The what, how, why, and when of dendrochemistry: (paleo)environmental information from the chemical analysis of tree rings G. Binda et al. 10.1016/j.scitotenv.2020.143672
32. An overview on isotopic divergences – causes for instability of tree-ring isotopes and climate correlations M. Savard & V. Daux 10.5194/cp-16-1223-2020
33. French summer droughts since 1326 AD: a reconstruction based on tree ring cellulose δ<sup>18</sup>O I. Labuhn et al. 10.5194/cpd-11-5113-2015