Abstract
Through its intimate connection with the El Niño/Southern Oscillation system, climate variability in the tropical Pacific Ocean influences climate across much of the planet. But the history of temperature change in the tropical Pacific Ocean during recent millennia is poorly known: the available annually resolved records1,2 are discontinuous and rarely span more than a few centuries. Longer records at coarser temporal resolution suggest that significant oceanographic changes, observed at multi-year to multi-century resolution, have had important effects on global climate3,4,5. Here we use a diatom record from El Junco Lake, Galápagos, to produce a calibrated, continuous record of sea surface temperature in the eastern tropical Pacific Ocean at subdecadal resolution, spanning the past 1,200 years. Our reconstruction reveals that the most recent 50 years are the warmest 50-year period within the record. Because our diatom-based sea surface temperature index resembles Northern Hemisphere temperature reconstructions, we suggest that with continued anthropogenic warming, the eastern tropical Pacific Ocean may continue to warm.
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References
Cobb, K. M., Charles, C. D., Cheng, H. & Edwards, R. L. El Niño/Southern Oscillation and tropical Pacific climate during the last millennium. Nature 424, 271–276 (2003).
Cole, J. E. in Global Change in the Holocene (eds McKay, A. et al.) 437–452 (Arnold, 2003).
Koutavas, A., Lynch-Stieglitz, J., Marchitto, T. M. & Sachs, J. P. El Niño-like pattern in ice age tropical Pacific sea surface temperature. Science 297, 226–230 (2002).
Rein, B. et al. El Niño variability off Peru during the last 20,000 years. Paleoceanography 20, PA4003 (2005).
Stott, L. et al. Decline of surface temperature and salinity in the western tropical Pacific Ocean in the Holocene epoch. Nature 431, 56–59 (2004).
Bjerknes, J. Atmospheric teleconnections from the equatorial Pacific. Mon. Weath. Rev. 97, 163–172 (1969).
Tribbia, J. J. in Teleconnections Linking Climate Anomalies Worldwide: Scientific Basis and Societal Impact (eds Glantz, M. H., Katz, R. W. & Nicholls, N.) 285–308 (Cambridge Univ. Press, 1991).
Vecchi, G. A. et al. Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing. Nature 441, 73–76 (2006).
Snell, H. & Rea, S. The 1997–98 El Niño in the Galápagos: Can 34 years of data estimate 120 years of pattern? Noticias de Galapagos 60, 11–20 (1999).
Conroy, J. L. et al. Holocene changes in eastern tropical Pacific climate inferred from a Galápagos lake sediment record. Quat. Sci. Rev. 27, 1166–1180 (2008).
Smith, T. M. & Reynolds, R. W. Improved extended reconstruction of SST (1854–1997). J. Clim. 17, 2466–2477 (2004).
Wolin, J. A. & Duthrie, H. C. in The Diatoms: Applications for the Environmental and Earth Sciences (eds Stoermer, E. F. & Smol, J. P.) 469 (Cambridge Univ. Press, 1999).
Schofield, E. K. & Colinvaux, P. A. Fossil Azolla from the Galápagos Islands. Bull. Torrey Botanical Club 96, 623–628 (1969).
McMullen, C. K. Flowering Plants of the Galapagos (Cornell Univ., 1999).
Moy, C. M., Seltzer, G. O., Rodbell, D. T. & Anderson, D. M. Variability of El Niño/Southern Oscillation activity at millennial timescales during the Holocene epoch. Nature 420, 162–165 (2002).
Koutavas, A., DeMenocal, P. B., Olive, G. C. & Lynch-Stieglitz, J. Mid-Holocene El Niño-Southern Oscillation (ENSO) attenuation revealed by individual foraminifera in eastern tropical Pacific sediments. Geology 34, 993–996 (2006).
Mitchell, T. P. & Wallace, J. M. The annual cycle in equatorial convection and sea-surface temperature. J. Clim. 5, 1140–1156 (1992).
Dunbar, R. B., Wellington, G. M., Colgan, M. W. & Glynn, P. W. Eastern Pacific SST since 1600 AD: The δ18O record of climate variability in Galápagos corals. Paleoceanography 9, 291–315 (1994).
Palacios, D. M. Seasonal patterns of sea-surface temperature and ocean color around the Galapagos: Regional and local influences. Deep-Sea Res. II 51, 43–57 (2004).
Clement, A. C., Seager, R., Cane, M. A. & Zebiak, S. E. An ocean dynamical thermostat. J Clim. 9, 2190–2196 (1996).
Mann, M. E., Cane, M. A., Zebiak, S. E. & Clement, A. Volcanic and solar forcing of the tropical Pacific over the past 1000 years. J. Clim. 18, 447–456 (2005).
Graham, N. E. et al. Tropical Pacific-mid-latitude teleconnections in medieval times. Clim. Change 83, 241–285 (2007).
Jansen, E. et al. in Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (eds Solomon, S. et al.) 433–496 (Cambridge Univ. Press, 2007).
Thompson, L. G. et al. Abrupt tropical climate change: Past and present. Proc. Natl Acad. Sci. USA 103, 10536–10543 (2006).
Thompson, L. G. et al. Late-Glacial stage and Holocene tropical ice core records from Huascarán, Peru. Science 269, 46–50 (1995).
Battarbee, R. W. New method for estimation of absolute microfossil numbers, with reference especially to diatoms. Limnol. Oceanogr. 18, 647–653 (1973).
Faegri, K., Kaland, P. E. & Krzywinski, K. Textbook of Pollen Analysis 4th edn (Wiley, 1989).
Baker, C. B., Eischeid, J. K., Karl, T. R. & Diaz, H. F. The Quality Control of Long-Term Climatological Data Using Objective Data Analysis (Dallas, 1994).
Acknowledgements
We are grateful for the field assistance of M. Miller, J. Weiss, H. Barnett, T. Damassa, B. Fonseca and R. Smittenberg. Thanks to A. Cohen and J. Sachs for valuable discussion and helpful comments, W. Gosling for Galápagos climate data and M. Brenner and Z. Zhang for chronological data. Special thanks to the Galápagos National Park and the Charles Darwin Research Station for logistic support, The University of Arizona Department of Geosciences for extra funding and the University of Arizona AMS Facility for radiocarbon dates. This research was financially supported in part by a National Science Foundation Graduate Research Fellowship, as well as a grant from the Climate Program Office of NOAA.
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P.A.C. first discovered El Junco, named the lake, and motivated the current research. P.A.C., J.T.O., J.E.C., M.B.B. and M.S.-K. planned the project. J.T.O., M.S.-K., J.L.C. and P.A.C. participated in the expedition to the Galápagos. J.T.O. and J.L.C. collected the sediment cores. J.L.C. developed the age model, collected the diatom data and wrote the paper. A.R. collected the pollen data. All authors commented on the manuscript and helped analyse the results.
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Conroy, J., Restrepo, A., Overpeck, J. et al. Unprecedented recent warming of surface temperatures in the eastern tropical Pacific Ocean. Nature Geosci 2, 46–50 (2009). https://doi.org/10.1038/ngeo390
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DOI: https://doi.org/10.1038/ngeo390
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