CLIMAP Project Members The surface of the Ice-Age Earth. Science 191, 1131–1137 (1976).
MARGO Project Members Constraints on the magnitude and patterns of ocean cooling at the Last Glacial Maximum. Nat. Geosci. 2, 127–132 (2009).
Charney, J. G. et al. Carbon Dioxide and Climate: A Scientific Assessment (National Academy of Sciences, 1979).
Knutti, R. & Hegerl, G. C. The equilibrium sensitivity of the Earth’s temperature to radiation changes. Nat. Geosci. 1, 735–743 (2008).
Joussaume, S. & Taylor, K. Status of the Paleoclimate Modeling Intercomparison Project (PMIP) (WMO, 1995).
Braconnot, P. et al. Evaluation of climate models using palaeoclimatic data. Nat. Clim. Change 2, 417–424 (2012).
Schmittner, A. et al. Climate sensitivity estimated from temperature reconstructions of the Last Glacial Maximum. Science 334, 1385–1388 (2011).
Mix, A. C., Morey, A. E., Pisias, N. G. & Hostetler, S. W. Foraminiferal faunal estimates of paleotemperature: circumventing the no-analog problem yields cool ice age tropics. Paleoceanography 14, 350–359 (1999).
Crowley, T. CLIMAP SSTs re-revisited. Clim. Dynam. 16, 241–255 (2000).
Ballantyne, A., Lavine, M., Crowley, T., Liu, J. & Baker, P. Meta-analysis of tropical surface temperatures during the Last Glacial Maximum. Geophys. Res. Lett. 32, L05712 (2005).
Telford, R., Li, C. & Kucera, M. Mismatch between the depth habitat of planktonic foraminifera and the calibration depth of SST transfer functions may bias reconstructions. Clim. Past 9, 859–870 (2013).
Tierney, J. E. & Tingley, M. P. BAYSPLINE: a new calibration for the alkenone paleothermometer. Paleoceanogr. Paleoclimatol. 33, 281–301 (2018).
Tierney, J. E., Malevich, S. B., Gray, W., Vetter, L. & Thirumalai, K. Bayesian calibration of the Mg/Ca paleothermometer in planktic foraminifera. Paleoceanogr. Paleoclimatol. 34, 2005–2030 (2019).
Snyder, C. W. Evolution of global temperature over the past two million years. Nature 538, 226–228 (2016).
Schneider von Deimling, T., Ganopolski, A., Held, H. & Rahmstorf, S. How cold was the Last Glacial Maximum? Geophys. Res. Lett. 33, L14709 (2006).
Holden, P. B., Edwards, N., Oliver, K., Lenton, T. & Wilkinson, R. A probabilistic calibration of climate sensitivity and terrestrial carbon change in GENIE-1. Clim. Dynam. 35, 785–806 (2010).
Shakun, J. D. et al. Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation. Nature 484, 49–54 (2012).
Annan, J. & Hargreaves, J. C. A new global reconstruction of temperature changes at the Last Glacial Maximum. Clim. Past 9, 367–376 (2013).
Bereiter, B., Shackleton, S., Baggenstos, D., Kawamura, K. & Severinghaus, J. Mean global ocean temperatures during the last glacial transition. Nature 553, 39–44 (2018).
Friedrich, T. & Timmermann, A. Using Late Pleistocene sea surface temperature reconstructions to constrain future greenhouse warming. Earth Planet. Sci. Lett. 530, 115911 (2020).
Masson-Delmotte, V. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) 383–464 (IPCC, Cambridge Univ. Press, 2013).
Brady, E. et al. The connected isotopic water cycle in the Community Earth System Model Version 1. J. Adv. Model. Earth Syst. 11, 2547–2566 (2019).
Tierney, J. E. & Tingley, M. P. A. Bayesian, spatially-varying calibration model for the TEX86 proxy. Geochim. Cosmochim. Acta 127, 83–106 (2014).
Malevich, S. B., Vetter, L. & Tierney, J. E. Global core top calibration of δ18O in planktic foraminifera to sea surface temperature. Paleoceanogr. Paleoclimatol. 34, 1292–1315 (2019).
Tardif, R. et al. Last millennium reanalysis with an expanded proxy database and seasonal proxy modeling. Clim. Past 15, 1251–1273 (2019).
Gray, W. R. et al. Wind-driven evolution of the North Pacific subpolar gyre over the last deglaciation. Geophys. Res. Lett. 47, e2019GL086328 (2020).
DiNezio, P. N. et al. Glacial changes in tropical climate amplified by the Indian Ocean. Sci. Adv. 4, eaat9658 (2018).
Ford, H. L., Ravelo, A. C. & Polissar, P. J. Reduced El Niño–Southern Oscillation during the Last Glacial Maximum. Science 347, 255–258 (2015).
Glushkova, O. Y. Geomorphological correlation of Late Pleistocene glacial complexes of Western and Eastern Beringia. Quat. Sci. Rev. 20, 405–417 (2001).
Bartlein, P. J. et al. Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis. Clim. Dynam. 37, 775–802 (2011).
Roe, G. H. & Lindzen, R. S. The mutual interaction between continental-scale ice sheets and atmospheric stationary waves. J. Clim. 14, 1450–1465 (2001).
Löfverström, M. & Liakka, J. On the limited ice intrusion in Alaska at the LGM. Geophys. Res. Lett. 43, 11030–11038 (2016).
Hopcroft, P. O. & Valdes, P. J. How well do simulated Last Glacial Maximum tropical temperatures constrain equilibrium climate sensitivity? Geophys. Res. Lett. 42, 5533–5539 (2015).
Porter, S. C. Snowline depression in the tropics during the Last Glaciation. Quat. Sci. Rev. 20, 1067–1091 (2000).
Stute, M. et al. Cooling of tropical Brazil (5 °C) during the Last Glacial Maximum. Science 269, 379–383 (1995).
Lea, D. W., Pak, D. K. & Spero, H. J. Climate impact of late Quaternary equatorial Pacific sea surface temperature variations. Science 289, 1719–1724 (2000).
Masson-Delmotte, V. et al. EPICA Dome C record of glacial and interglacial intensities. Quat. Sci. Rev. 29, 113–128 (2010).
Lee, J.-E., Fung, I., DePaolo, D. J. & Otto-Bliesner, B. Water isotopes during the Last Glacial Maximum: new general circulation model calculations. J. Geophys. Res. 113, D19109 (2008).
Kurahashi-Nakamura, T., Paul, A. & Losch, M. Dynamical reconstruction of the global ocean state during the Last Glacial Maximum. Paleoceanography 32, 326–350 (2017).
Amrhein, D. E., Wunsch, C., Marchal, O. & Forget, G. A global glacial ocean state estimate constrained by upper-ocean temperature proxies. J. Clim. 31, 8059–8079 (2018).
Flato, G. et al. in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) 741–866 (IPCC, Cambridge Univ. Press, 2014).
PALAEOSENS Project Members Making sense of palaeoclimate sensitivity. Nature 491, 683–691 (2012); erratum 494, 130 (2013).
Prentice, I. C., Jolly, D. & Biome 6000 Participants Mid-Holocene and glacial-maximum vegetation geography of the northern continents and Africa. J. Biogeogr. 27, 507–519 (2000).
Köhler, P. et al. What caused Earth’s temperature variations during the last 800,000 years? Data-based evidence on radiative forcing and constraints on climate sensitivity. Quat. Sci. Rev. 29, 129–145 (2010).
Etminan, M., Myhre, G., Highwood, E. & Shine, K. Radiative forcing of carbon dioxide, methane, and nitrous oxide: a significant revision of the methane radiative forcing. Geophys. Res. Lett. 43, 12614–12623 (2016).
Albani, S. et al. Aerosol-climate interactions during the Last Glacial Maximum. Curr. Clim. Change Rep. 4, 99–114 (2018).
Shakun, J. D. Modest global-scale cooling despite extensive early Pleistocene ice sheets. Quat. Sci. Rev. 165, 25–30 (2017).
Stap, L., Köhler, P. & Lohmann, G. Including the efficacy of land ice changes in deriving climate sensitivity from paleodata. Earth Syst. Dynam. 10, 333–345 (2019).
Yoshimori, M., Yokohata, T. & Abe-Ouchi, A. A comparison of climate feedback strength between CO2 doubling and LGM experiments. J. Clim. 22, 3374–3395 (2009).
Friedrich, T., Timmermann, A., Tigchelaar, M., Timm, O. E. & Ganopolski, A. Nonlinear climate sensitivity and its implications for future greenhouse warming. Sci. Adv. 2, e1501923 (2016).
DiNezio, P. N. & Tierney, J. E. The effect of sea level on glacial Indo-Pacific climate. Nat. Geosci. 6, 485–491 (2013).
Chan, D., Kent, E. C., Berry, D. I. & Huybers, P. Correcting datasets leads to more homogeneous early-twentieth-century sea surface warming. Nature 571, 393–397 (2019).
Reimer, P. J. et al. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55, 1869–1887 (2013).
Hurrell, J. W. et al. The community earth system model: a framework for collaborative research. Bull. Am. Meteorol. Soc. 94, 1339–1360 (2013).
Kageyama, M. et al. The PMIP4 contribution to CMIP6–Part 4: scientific objectives and experimental design of the PMIP4-CMIP6 Last Glacial Maximum experiments and PMIP4 sensitivity experiments. Geosci. Model Dev. 10, 4035–4055 (2017).
Peltier, W. R., Argus, D. F. & Drummond, R. Space geodesy constrains ice age terminal deglaciation: the global ICE-6G_C (VM5a) model. J. Geophys. Res. Solid Earth 120, 450–487 (2015).
Lawrence, D. M. et al. Parameterization improvements and functional and structural advances in version 4 of the community land model. J. Adv. Model. Earth Syst. 3, M03001 (2011).
Zhu, J. et al. Reduced ENSO variability at the LGM revealed by an isotope-enabled Earth system model. Geophys. Res. Lett. 44, 6984–6992 (2017).
Gettelman, A., Kay, J. E. & Shell, K. M. The evolution of climate sensitivity and climate feedbacks in the Community Atmosphere Model. J. Clim. 25, 1453–1469 (2012).
Zhu, J., Poulsen, C. J. & Tierney, J. E. Simulation of Eocene extreme warmth and high climate sensitivity through cloud feedbacks. Sci. Adv. 5, eeax1874 (2019).
Richardson, A. D. et al. Climate change, phenology, and phenological control of vegetation feedbacks to the climate system. Agric. For. Meteorol. 169, 156–173 (2013).
Meehl, G. A. et al. Effects of model resolution, physics, and coupling on Southern Hemisphere storm tracks in CESM1.3. Geophys. Res. Lett. 46, 12408–12416 (2019).
Whitaker, J. S. & Hamill, T. M. Ensemble data assimilation without perturbed observations. Mon. Weath. Rev. 130, 1913–1924 (2002).
Steiger, N. J., Hakim, G. J., Steig, E. J., Battisti, D. S. & Roe, G. H. Assimilation of time-averaged pseudoproxies for climate reconstruction. J. Clim. 27, 426–441 (2014).
Hakim, G. J. et al. The last millennium climate reanalysis project: framework and first results. J. Geophys. Res. Atmos. 121, 6745–6764 (2016).
Okazaki, A. & Yoshimura, K. Development and evaluation of a system of proxy data assimilation for paleoclimate reconstruction. Clim. Past 13, 379–393 (2017).
Lauvset, S. K. et al. A new global interior ocean mapped climatology: the 1 × 1 GLODAP version 2. Earth Syst. Sci. Data 8, 325–340 (2016).
Gray, W. R. & Evans, D. Nonthermal influences on Mg/Ca in planktonic foraminifera: a review of culture studies and application to the last glacial maximum. Paleoceanogr. Paleoclimatol. 34, 306–315 (2019).
Houtekamer, P. L. & Mitchell, H. L. A sequential ensemble Kalman filter for atmospheric data assimilation. Mon. Weath. Rev. 129, 123–137 (2001).
Gaspari, G. & Cohn, S. E. Construction of correlation functions in two and three dimensions. Q. J. R. Meteorol. Soc. 125, 723–757 (1999).
Nash, J. E. & Sutcliffe, J. V. River flow forecasting through conceptual models part I—a discussion of principles. J. Hydrol. 10, 282–290 (1970).
Werner, M. et al. Glacial–interglacial changes of H2 18O, HDO and deuterium excess—results from the fully coupled Earth System Model ECHAM5/MPI-OM. Geosci. Model Dev. 9, 647–670 (2016).
Atsawawaranunt, K. et al. The SISAL database: a global resource to document oxygen and carbon isotope records from speleothems. Earth Syst. Sci. Data 10, 1687–1713 (2018).
Comas-Bru, L. et al. Evaluating model outputs using integrated global speleothem records of climate change since the last glacial. Clim. Past 15, 1557–1579 (2019).
Hamill, T. M. Interpretation of rank histograms for verifying ensemble forecasts. Mon. Weath. Rev. 129, 550–560 (2001).
Danabasoglu, G. et al. The CCSM4 ocean component. J. Clim. 25, 1361–1389 (2012).
Park, T.-W., Deng, Y., Cai, M., Jeong, J.-H. & Zhou, R. A dissection of the surface temperature biases in the Community Earth System Model. Clim. Dynam. 43, 2043–2059 (2014).
Taylor, K. et al. Estimating shortwave radiative forcing and response in climate models. J. Clim. 20, 2530–2543 (2007).
Braconnot, P. & Kageyama, M. Shortwave forcing and feedbacks in Last Glacial Maximum and Mid-Holocene PMIP3 simulations. Phil. Trans. R. Soc. A 373, 20140424 (2015).
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