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A Walker switch mechanism driving millennial-scale climate variability

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  • Corresponding author: paul.wilcox@uibk.ac.at (P.W.) 
    1. We present a high-resolution speleothem δ18O record from southeastern Alaska covering the past 13,500 years.

      The record shows an equatorial Pacific climate pattern and is at odds with North Atlantic climate patterns, questioning the bipolar seesaw mechanism as the source of global climate variability.

      We propose a new climate mechanism originating in the equatorial Pacific that could explain millennial-scale climate variability on Earth.

  • A key goal of paleoclimate science is to identify the source of millennial-scale climate fluctuations. Although long-term changes in the Earth’s position relative to the Sun are the driver of climate change on timescales of ≥ 19 thousand years (ka), it is still incompletely understood what causes rapid sub-orbital changes in climate that were common during glacial periods. Here, we provide a continuous, precisely dated speleothem record from southeastern Alaska that spans the last 13.5 ka. Despite its location in the high latitudes of the Northern Hemisphere, this record shows an equatorial Pacific climate pattern during the end of the last deglaciation and Holocene, and is at odds with North Atlantic climate patterns, calling into question the bipolar seesaw mechanism for the Pacific realm. Because of this, we propose a new mechanism to account for sub-orbitally forced climate changes. The mechanism, termed the Walker switch, is forced by insolation and results in rapid zonal sea-surface temperature changes in the equatorial Pacific. The climatic effects of the Walker switch are propagated across the globe, including the high northern latitudes.
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  • [1] Denton, G.H., Toucanne, S., Putnam, A.E., et al. (2022). Heinrich summers. Quat. Sci. Rev. 295, 107750.

    View in Article CrossRef Google Scholar

    [2] Heinrich, H. (1988). Origin and consequences of cyclic ice rafting in the Northeast Atlantic Ocean during the past 130,000 years. Quat. Res. 29, 142−152.

    View in Article CrossRef Google Scholar

    [3] Stocker, T.F. (1998). The seesaw effect. Science 282, 61−62.

    View in Article CrossRef Google Scholar

    [4] Marino, G., Rohling, E.J., Rodríguez-Sanz, L., et al. (2015). Bipolar seesaw control on last interglacial sea level. Nature 522, 197−201.

    View in Article CrossRef Google Scholar

    [5] Wolff, E.W., Chappellaz, J., Blunier, T., et al. (2010). Millennial-scale variability during the last glacial: The ice core record. Quat. Sci. Rev. 29, 2828−2838.

    View in Article CrossRef Google Scholar

    [6] Davis, C.V., Myhre, S.E., Deutsch, C., et al. (2020). Sea surface temperature across the Subarctic North Pacific and marginal seas through the past 20,000 years: A paleoceanographic synthesis. Quat. Sci. Rev. 246, 106519.

    View in Article CrossRef Google Scholar

    [7] Praetorius, S.K., and Mix, A.C. (2014). Synchronization of North Pacific and Greenland climates preceded abrupt deglacial warming. Science 345, 444−448.

    View in Article CrossRef Google Scholar

    [8] Davies, M.H., Mix, A.C., Stoner, J.S., et al. (2011). The deglacial transition on the southeastern Alaska Margin: Meltwater input, sea level rise, marine productivity, and sedimentary anoxia. Paleoceanography 26, PA2223.

    View in Article Google Scholar

    [9] Praetorius, S.K., Condron, A., Mix, A.C., et al. (2020). The role of Northeast Pacific meltwater events in deglacial climate change. Sci. Adv. 6, eaay2915.

    View in Article CrossRef Google Scholar

    [10] Wilcox, P.S., Mundelsee, M., Spötl, C., et al. (2023). Anthropogenically forced shift in ENSO mean state after 1970 CE. Authorea. 10.22541/essoar.168882026.60869658/v1.

    View in Article Google Scholar

    [11] Liu, Z., and Alexander, M. (2007). Atmospheric bridge, oceanic tunnel, and global climatic teleconnections. Rev. Geophys. 45, RG2005.

    View in Article Google Scholar

    [12] Clement, A.C., Seager, R., Cane, M.A., and Zebiak, S.E. (1996). An ocean dynamical thermostat. J. Clim. 9, 2190−2196.

    View in Article CrossRef Google Scholar

    [13] Koutavas, A., and Joanides, S. (2012). El Niño–Southern oscillation extrema in the Holocene and last glacial maximum. Paleoceanography 27, PA4208.

    View in Article Google Scholar

    [14] Sadekov, A.Y., Ganeshram, R., Pichevin, L., et al. (2013). Palaeoclimate reconstructions reveal a strong link between El Niño-Southern Oscillation and Tropical Pacific mean state. Nat. Commun. 4, 2692.

    View in Article CrossRef Google Scholar

    [15] Cane, M.A. (1998). A role for the tropical Pacific. Science 282, 59−61.

    View in Article CrossRef Google Scholar

    [16] Kubota, K., Yokoyama, Y., Ishikawa, T., et al. (2014). Larger CO2 source at the equatorial Pacific during the last deglaciation. Sci. Rep. 4, 5261.

    View in Article CrossRef Google Scholar

    [17] Feely, R.A., Wanninkhof, R., Takahashi, T., and Tans, P. (1999). Influence of El Niño on the equatorial Pacific contribution to atmospheric CO2 accumulation. Nature 398, 597−601.

    View in Article CrossRef Google Scholar

    [18] Chatterjee, A., Gierach, M.M., Sutton, A.J., et al. (2017). Influence of El Niño on atmospheric CO2 over the tropical Pacific Ocean: Findings from NASA’s OCO-2 mission. Science 358, eaam5776.

    View in Article CrossRef Google Scholar

    [19] Takahashi, T., Sutherland, S.C., Wanninkhof, R., et al. (2009). Climatological mean and decadal change in surface ocean pCO2, and net sea–air CO2 flux over the global oceans. Deep Sea Res. Part II: Top. Stud. Oceanogr. 56, 554−577.

    View in Article CrossRef Google Scholar

    [20] Vecchi, G.A., and Soden, B.J. (2007). Global warming and the weakening of the tropical circulation. J. Clim. 20, 4316−4340.

    View in Article CrossRef Google Scholar

    [21] Misios, S., Gray, L.J., Knudsen, M.F., et al. (2019). Slowdown of the Walker circulation at solar cycle maximum. Proc. Natl. Acad. Sci. U.S.A. 116, 7186−7191.

    View in Article CrossRef Google Scholar

    [22] Moy, C.M., Seltzer, G.O., Rodbell, D.T., and Anderson, D.M. (2002). Variability of El Niño/Southern Oscillation activity at millennial timescales during the Holocene epoch. Nature 420, 162−165.

    View in Article CrossRef Google Scholar

    [23] Conroy, J.L., Overpeck, J.T., Cole, J.E., et al. (2008). Holocene changes in eastern tropical Pacific climate inferred from a Galápagos lake sediment record. Quat. Sci. Rev. 27, 1166−1180.

    View in Article CrossRef Google Scholar

    [24] Haug, G.H., Hughen, K.A., Sigman, D.M., et al. (2001). Southward migration of the intertropical convergence zone through the Holocene. Science 293, 1304−1308.

    View in Article CrossRef Google Scholar

    [25] Walczak, M.H., Mix, A.C., Cowan, E.A., et al. (2020). Phasing of millennial-scale climate variability in the Pacific and Atlantic Oceans. Science 370, 716−720.

    View in Article Google Scholar

    [26] Tarasov, L., and Peltier, W.R. (2005). Arctic freshwater forcing of the Younger Dryas cold reversal. Nature 435, 662−665.

    View in Article CrossRef Google Scholar

    [27] Kokorowski, H.D., Anderson, P.M., Mock, C.J., and Lozhkin, A.V. (2008). A re-evaluation and spatial analysis of evidence for a Younger Dryas climatic reversal in Beringia. Quat. Sci. Rev. 27, 1710−1722.

    View in Article CrossRef Google Scholar

    [28] Kielhofer, J.R., Tierney, J.E., Reuther, J.D., et al. (2023). BrGDGT temperature reconstruction from interior Alaska: Assessing 14,000 years of deglacial to Holocene temperature variability and potential effects on early human settlement. Quat. Sci. Rev. 303, 107979.

    View in Article CrossRef Google Scholar

    [29] Vecchi, G.A., Soden, B.J., Wittenberg, A.T., et al. (2006). Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing. Nature 441, 73−76.

    View in Article CrossRef Google Scholar

    [30] Bereiter, B., Eggleston, S., Schmitt, J., et al. (2015). Revision of the EPICA Dome C CO2 record from 800 to 600 kyr before present. Geophys. Res. Lett. 42, 542−549.

    View in Article CrossRef Google Scholar

    [31] Berger, A. (1978). Long-term variations of daily insolation and Quaternary climatic changes. J. Atmos. Sci. 35, 2362−2367.

    View in Article CrossRef Google Scholar

    [32] Jouzel, J., Masson-Delmotte, V., Cattani, O., et al. (2007). Orbital and millennial Antarctic climate variability over the past 800,000 years. Science 317, 793−796.

    View in Article CrossRef Google Scholar

    [33] Cheng, H., Edwards, R.L., Sinha, A., et al. (2016). The Asian monsoon over the past 640,000 years and ice age terminations. Nature 534, 640−646.

    View in Article CrossRef Google Scholar

  • Cite this article:

    Wilcox P., Spötl C., Honkonen J., et al., (2023). A Walker switch mechanism driving millennial-scale climate variability. The Innovation Geoscience 1(2), 100026. https://doi.org/10.59717/j.xinn-geo.2023.100026
    Wilcox P., Spötl C., Honkonen J., et al., (2023). A Walker switch mechanism driving millennial-scale climate variability. The Innovation Geoscience 1(2), 100026. https://doi.org/10.59717/j.xinn-geo.2023.100026

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