Hemming, S. R. Heinrich events: massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint. Rev. Geophys. 42, RG1005 (2004).
Bauska, T. K. et al. Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation. Proc. Natl Acad. Sci. USA 113, 3465–3470 (2016).
Stríkis, N. M. et al. South American monsoon response to iceberg discharge in the North Atlantic. Proc. Natl Acad. Sci. USA 115, 3788–3793 (2018).
Nguyen, D. C. et al. Precipitation response to Heinrich Event-3 in the northern Indochina as revealed in a high-resolution speleothem record. J. Asian Earth Sci. X 7, 100090 (2022).
Henry, L. G. et al. North Atlantic ocean circulation and abrupt climate change during the last glaciation. Science 353, 470–474 (2016).
Barker, S. et al. Icebergs not the trigger for North Atlantic cold events. Nature 520, 333–336 (2015).
Lynch-Stieglitz, J. The Atlantic Meridional Overturning Circulation and abrupt climate change. Ann. Rev. Mar. Sci. 9, 83–104 (2017).
Capron, E. et al. The anatomy of past abrupt warmings recorded in Greenland ice. Nat. Commun. 12, 2106 (2021).
Buizert, C. et al. Abrupt ice-age shifts in southern westerly winds and Antarctic climate forced from the north. Nature 563, 681–685 (2018).
Pedro, J. B. et al. Beyond the bipolar seesaw: toward a process understanding of interhemispheric coupling. Quat. Sci. Rev. 192, 27–46 (2018).
Hodell, D. A. et al. Anatomy of Heinrich Layer 1 and its role in the last deglaciation. Paleoceanography 32, 284–303 (2017).
Barker, S. et al. Interhemispheric Atlantic seesaw response during the last deglaciation. Nature 457, 1097–1102 (2009).
Dong, X. et al. Coupled atmosphere–ice–ocean dynamics during Heinrich Stadial 2. Nat. Commun. 13, 5867 (2022).
Marcott, S. A. et al. Ice-shelf collapse from subsurface warming as a trigger for Heinrich events. Proc. Natl Acad. Sci. USA 108, 13415–13419 (2011).
Max, L., Nürnberg, D., Chiessi, C. M., Lenz, M. M. & Mulitza, S. Subsurface ocean warming preceded Heinrich events. Nat. Commun. 13, 4217 (2022).
Yang, X., Rial, J. A. & Reischmann, E. P. On the bipolar origin of Heinrich events. Geophys. Res. Lett. 41, 9080–9086 (2014).
Rhodes, R. H. et al. Enhanced tropical methane production in response to iceberg discharge in the North Atlantic. Science 348, 1016–1019 (2015).
Cheng, H., Sinha, A., Wang, X., Cruz, F. W. & Edwards, R. L. The Global Paleomonsoon as seen through speleothem records from Asia and the Americas. Clim. Dyn. 39, 1045–1062 (2012).
Deplazes, G. et al. Links between tropical rainfall and North Atlantic climate during the last glacial period. Nat. Geosci. 6, 213–217 (2013).
He, C. et al. Abrupt Heinrich Stadial 1 cooling missing in Greenland oxygen isotopes. Sci. Adv. 7, eabh1007 (2021).
Landais, A. et al. A review of the bipolar see-saw from synchronized and high resolution ice core water stable isotope records from Greenland and East Antarctica. Quat. Sci. Rev. 114, 18–32 (2015).
Severinghaus, J. P., Sowers, T., Brook, E. J., Alley, R. B. & Bender, M. L. Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice. Nature 391, 141–146 (1998).
Lee, J. E. et al. Excess methane in Greenland ice cores associated with high dust concentrations. Geochim. Cosmochim. Acta 270, 409–430 (2020).
Buizert, C. et al. The WAIS Divide deep ice core WD2014 chronology—Part 1: methane synchronization (68–31 ka bp) and the gas age–ice age difference. Clim. Past 11, 153–173 (2015).
Sigl, M. et al. The WAIS Divide deep ice core WD2014 chronology—Part 2: annual-layer counting (0–31 ka bp). Clim. Past 12, 769–786 (2016).
Seierstad, I. K. et al. Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint. Quat. Sci. Rev. 106, 29–46 (2014).
Svensson, A. et al. Bipolar volcanic synchronization of abrupt climate change in Greenland and Antarctic ice cores during the last glacial period. Clim. Past 16, 1565–1580 (2020).
Buizert, C. The ice core gas age–ice age difference as a proxy for surface temperature. Geophys. Res. Lett. 48, e2021GL094241 (2021).
Buizert, C. et al. Antarctic surface temperature and elevation during the Last Glacial Maximum. Science 372, 1097–1101 (2021).
Kindler, P. et al. Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core. Clim. Past 10, 887–902 (2014).
Kobashi, T. et al. High variability of Greenland surface temperature over the past 4000 years estimated from trapped air in an ice core. Geophys. Res. Lett. 38, 4–9 (2011).
Menviel, L. C., Skinner, L. C., Tarasov, L. & Tzedakis, P. C. An ice–climate oscillatory framework for Dansgaard–Oeschger cycles. Nat. Rev. Earth Environ. 1, 677–693 (2020).
Ziemen, F. A., Kapsch, M. L., Klockmann, M. & Mikolajewicz, U. Heinrich events show two-stage climate response in transient glacial simulations. Clim. Past 15, 153–168 (2019).
Badgeley, J. A., Steig, E. J., Hakim, G. J. & Fudge, T. J. Greenland temperature and precipitation over the last 20 000 years using data assimilation. Clim. Past 16, 1325–1346 (2020).
Bard, E., Rostek, F., Turon, J. L. & Gendreau, S. Hydrological impact of Heinrich events in the subtropical northeast Atlantic. Science 289, 1321–1324 (2000).
Pedro, J. B. et al. Dansgaard–Oeschger and Heinrich event temperature anomalies in the North Atlantic set by sea ice, frontal position and thermocline structure. Quat. Sci. Rev. 289, 107599 (2022).
Böhm, E. et al. Strong and deep Atlantic meridional overturning circulation during the last glacial cycle. Nature 517, 73–76 (2015).
Mayewski, P. A. et al. Major features and forcing of high-latitude Northern Hemisphere atmospheric circulation using a 110,000-year-long glaciochemical series. J. Geophys. Res. Ocean 102, 26345–26366 (1997).
Cheng, H. et al. The Asian monsoon over the past 640,000 years and ice age terminations. Nature 534, 640–646 (2016).
Bauska, T. K., Marcott, S. A. & Brook, E. J. Abrupt changes in the global carbon cycle during the last glacial period. Nat. Geosci. 14, 91–96 (2021).
McConnell, J. R. et al. Synchronous volcanic eruptions and abrupt climate change ~17.7 ka plausibly linked by stratospheric ozone depletion. Proc. Natl Acad. Sci. USA 114, 10035–10040 (2017).
Ceppi, P., Hwang, Y. T., Liu, X., Frierson, D. M. W. & Hartmann, D. L. The relationship between the ITCZ and the Southern Hemispheric eddy-driven jet. J. Geophys. Res. Atmos. 118, 5136–5146 (2013).
Ferrari, R. et al. Antarctic sea ice control on ocean circulation in present and glacial climates. Proc. Natl Acad. Sci. USA 111, 8753–8758 (2014).
Menviel, L. et al. Southern Hemisphere westerlies as a driver of the early deglacial atmospheric CO2 rise. Nat. Commun. 9, 2503 (2018).
Menviel, L., England, M. H., Meissner, K. J., Mouchet, A. & Yu, J. Atlantic–Pacific seesaw and its role in outgassing CO2 during Heinrich events. Paleoceanography 29, 58–70 (2014).
Rasmussen, S. O. et al. A stratigraphic framework for abrupt climatic changes during the last glacial period based on three synchronized Greenland ice-core records: refining and extending the INTIMATE event stratigraphy. Quat. Sci. Rev. 106, 14–28 (2014).
Clement, A. C. & Cane, M. in Mechanisms of Global Climate Change at Millennial Time Scales Geophysical Monograph Series Vol. 112 (eds Clark, P. U. et al.) 363–371 (AGU, 1999).
Johnsen, S. J. et al. The δ18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability. J. Geophys. Res. Ocean 102, 26397–26410 (1997).
Steig, E. J. et al. Continuous-flow analysis of δ17O, δ18O, and δD of H2O on an ice core from the South Pole. Front. Earth Sci. 9, 640292 (2021).
McManus, J. F., Francois, R., Gherardl, J. M., Kelgwin, L. & Drown-Leger, S. Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes. Nature 428, 834–837 (2004).
Wang, Y. J. et al. A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China. Science 294, 2345–2348 (2001).
Mudelsee, M. Ramp function regression: a tool for quantifying climate transitions. Comput. Geosci. 26, 293–307 (2000).
Mitchell, L. E., Brook, E. J., Sowers, T., McConnell, J. R. & Taylor, K. Multidecadal variability of atmospheric methane, 1000–1800 C.E. J. Geophys. Res. Biogeosci. 116, G02007 (2011).
Mitchell, L., Brook, E., Lee, J. E., Buizert, C. & Sowers, T. Constraints on the late Holocene anthropogenic contribution to the atmospheric methane budget. Science 342, 964–966 (2013).
Sowers, T., Bender, M. & Raynaud, D. Elemental and isotopic composition of occluded O2 and N2 in polar ice. J. Geophys. Res. 94, 5137–5150 (1989).
Petrenko, V. V., Severinghaus, J. P., Brook, E. J., Reeh, N. & Schaefer, H. Gas records from the West Greenland ice margin covering the Last Glacial Termination: a horizontal ice core. Quat. Sci. Rev. 25, 865–875 (2006).
Severinghaus, J., Beaudette, R., Headly, M., Taylor, K. & Brook, E. Oxygen-18 of O2 records the impact of abrupt climate change on the terrestrial biosphere. Science 324, 1431–1435 (2009).
Severinghaus, J. P. & Brook, E. J. Abrupt climate change at the end of the last glacial period inferred from trapped air in polar ice. Science 286, 930–934 (1999).
Grachev, A. M., Brook, E. J. & Severinghaus, J. P. Abrupt changes in atmospheric methane at the MIS 5b–5a transition. Geophys. Res. Lett. 34, L20703 (2007).
Kobashi, T., Severinghaus, J. P. & Kawamura, K. Argon and nitrogen isotopes of trapped air in the GISP2 ice core during the Holocene epoch (0–11,500 B.P.): methodology and implications for gas loss processes. Geochim. Cosmochim. Acta 72, 4675–4686 (2008).
Blunier, T. & Brook, E. J. Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period. Science 291, 109–112 (2001).
EPICA Community Members One-to-one coupling of glacial climate variability in Greenland and Antarctica. Nature 444, 195–198 (2006).
Epifanio, J. A. et al. The SP19 chronology for the South Pole ice core—Part 2: gas chronology, Δage, and smoothing of atmospheric records. Clim. Past 16, 2431–2444 (2020).
Bender, M. et al. Climate correlations between Greenland and Antarctica during the past 100,000 years. Nature 372, 663–666 (1994).
Severi, M. et al. Synchronisation of the EDML and EDC ice cores for the last 52 kyr by volcanic signature matching. Clim. Past 3, 367–374 (2007).
Severi, M., Udisti, R., Becagli, S., Stenni, B. & Traversi, R. Volcanic synchronisation of the EPICA-DC and TALDICE ice cores for the last 42 kyr bp. Clim. Past 8, 509–517 (2012).
Veres, D. et al. The Antarctic Ice Core Chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years. Clim. Past 9, 1733–1748 (2013).
Bazin, L. et al. An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka. Clim. Past 9, 1715–1731 (2013).
Rasmussen, S. O. et al. A new Greenland ice core chronology for the last glacial termination. J. Geophys. Res. Atmos. 111, D06102 (2006).
Andersen, K. K. et al. The Greenland Ice Core Chronology 2005, 15–42 ka. Part 1: constructing the time scale. Quat. Sci. Rev. 25, 3246–3257 (2006).
Svensson, A. et al. The Greenland Ice Core Chronology 2005, 15–42 ka. Part 2: comparison to other records. Quat. Sci. Rev. 25, 3258–3267 (2006).
Buizert, C. et al. Greenland temperature response to climate forcing during the last deglaciation. Science 345, 1177–1180 (2014).
Herron, B. M. M. & Langway, C. C. Firn densification: an empirical model. J. Glaciol. 25, 373–385 (1980).
Calonne, N. et al. Thermal conductivity of snow, firn, and porous ice from 3-D image-based computations. Geophys. Res. Lett. 46, 13079–13089 (2019).
Martinerie, P. et al. Air content paleo record in the Vostok ice core (Antarctica): a mixed record of climatic and glaciological parameters. J. Geophys. Res. 99, 10565–10576 (1994).
Blunier, T. & Schwander, J. Gas enclosure in ice: age difference and fractionation. In Physics of Ice Core Records, edited by: Hondoh, T., Hokkaido University Press, Sapporo, 307–326 (2000).
Rosen, J. L. et al. An ice core record of near-synchronous global climate changes at the Bølling transition. Nat. Geosci. 7, 459–463 (2014).
Orsi, A. J. Temperature Reconstruction at the West Antarctic Ice Sheet Divide, for the Last Millennium, from the Combination of Borehole Temperature and Inert Gas Isotope Measurements. DPhil dissertation, Univ. California, San Diego (2013); https://escholarship.org/uc/item/02g3c5fq.
Kobashi, T. et al. Persistent multi-decadal Greenland temperature fluctuation through the last millennium. Climatic Change 100, 733–756 (2010).
Buizert, C. et al. Precise interpolar phasing of abrupt climate change during the last ice age. Nature 520, 661–665 (2015).
Mudelsee, M. Break function regression: a tool for quantifying trend changes in climate time series. Eur. Phys. J. Spec. Top. 174, 49–63 (2009).
Lisiecki, L. E. & Stern, J. V. Regional and global benthic δ18O stacks for the last glacial cycle. Paleoceanography 31, 1368–1394 (2016).
Dahl-Jensen, D. et al. Eemian interglacial reconstructed from a Greenland folded ice core. Nature 493, 489–494 (2013).
Erhardt, T. et al. Decadal-scale progression of the onset of Dansgaard–Oeschger warming events. Clim. Past 15, 811–825 (2019).
Cuffey, K. M. & Clow, G. D. Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition. J. Geophys. Res. Ocean. 102, 26383–26396 (1997).
Buizert, C. et al. Greenland-wide seasonal temperatures during the last deglaciation. Geophys. Res. Lett. 45, 1905–1914 (2018).
Liu, Z. et al. Transient simulation of last deglaciation with a new mechanism for Bølling–Allerød warming. Science 325, 310–314 (2009).
Obase, T. & Abe-Ouchi, A. Abrupt Bølling–Allerød warming simulated under gradual forcing of the last deglaciation. Geophys. Res. Lett. 46, 11397–11405 (2019).
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