26 citations as recorded by crossref.

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2. Strategies for reducing the climate noise in model simulations: ensemble runs versus a long continuous run D. Decremer et al. 10.1007/s00382-014-2161-1
3. Deciphering Temperature Seasonality in Earth's Ancient Oceans L. Ivany & E. Judd 10.1146/annurev-earth-032320-095156
4. ENSO Variability During the Medieval Climate Anomaly as Recorded by Porites Corals From the Northern South China Sea L. Jiang et al. 10.1029/2020PA004173
5. Molluscan isotope sclerochronology in marine palaeoclimatology: Taxa, technique and timespan issues A. Johnson et al. 10.1016/j.quascirev.2024.109068
6. Coral‐Derived Western Pacific Tropical Sea Surface Temperatures During the Last Millennium T. Chen et al. 10.1002/2018GL077619
7. Comparison of model noise in AGCM independent ensemble runs and continuous simulation D. Decremer & C. Chung 10.1007/s13143-014-0014-9
8. Paleoclimate Proxies and the Benefits of Disunity A. Watkins 10.1017/psa.2024.12
9. Towards an understanding of climate proxy formation in the Chew Bahir basin, southern Ethiopian Rift V. Foerster et al. 10.1016/j.palaeo.2018.04.009
10. Modern drought conditions in western Sahel unprecedented in the past 1600 years M. Carré et al. 10.1007/s00382-018-4311-3
11. Holocene ENSO variability in the South China Sea recorded by high-resolution oxygen isotope records from the shells of Tridacna spp. D. Shao et al. 10.1038/s41598-020-61013-2
12. A Simple Monte Carlo Approach to Estimate the Uncertainties of SST and δ18Osw Inferred From Coral Proxies T. Watanabe & M. Pfeiffer 10.1029/2021GC009813
13. Quantifying Structural Uncertainty in Paleoclimate Data Assimilation With an Application to the Last Millennium D. Amrhein et al. 10.1029/2020GL090485
14. Quantifying errors in coral-based ENSO estimates: Toward improved forward modeling ofδ18O S. Stevenson et al. 10.1002/palo.20059
15. Reconstructing El Ni?o-Southern Oscillation activity and ocean temperature seasonality from short-lived marine mollusk shells from Peru M. Carr et al. 10.1016/j.palaeo.2012.12.014
16. Investigating the influence of temperature and seawater δ18O on Donax obesulus (Reeve, 1854) shell δ18O J. Warner et al. 10.1016/j.chemgeo.2021.120638
17. Reevaluating the Little Ice Age: Novel insights from oceanic and terrestrial records on unexpected warm winters H. Guo et al. 10.1016/j.quascirev.2024.108527
18. Simple noise estimates and pseudoproxies for the last 21 000 years O. Bothe et al. 10.5194/essd-11-1129-2019
19. Links between tropical Pacific seasonal, interannual and orbital variability during the Holocene J. Emile-Geay et al. 10.1038/ngeo2608
20. Summer Temperature over the Tibetan Plateau Modulated by Atlantic Multidecadal Variability C. Shi et al. 10.1175/JCLI-D-17-0858.1
21. CO2 capture and storage: A way forward for sustainable environment M. Anwar et al. 10.1016/j.jenvman.2018.08.009
22. A ~700 years perspective on the 21st century drying in the eastern part of Europe based on δ18O in tree ring cellulose V. Nagavciuc et al. 10.1038/s43247-022-00605-4
23. Positive precipitation–evaporation budget from AD 460 to 1090 in the Saloum Delta (Senegal) indicated by mollusk oxygen isotopes M. Azzoug et al. 10.1016/j.gloplacha.2012.08.003
24. High-resolution marine data and transient simulations support orbital forcing of ENSO amplitude since the mid-Holocene M. Carré et al. 10.1016/j.quascirev.2021.107125
25. Significantly lower summer minimum temperature warming trend on the southern Tibetan Plateau than over the Eurasian continent since the Industrial Revolution C. Shi et al. 10.1088/1748-9326/ab55fc
26. Holocene history of ENSO variance and asymmetry in the eastern tropical Pacific M. Carré et al. 10.1126/science.1252220