TY - JOUR
T1 - Unprecedented recent warming of surface temperatures in the eastern tropical Pacific Ocean
AU - Conroy, Jessica L.
AU - Restrepo, Alejandra
AU - Overpeck, Jonathan T.
AU - Steinitz-Kannan, Miriam
AU - Cole, Julia E.
AU - Bush, Mark B.
AU - Colinvaux, Paul A.
N1 - Funding Information:
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.
PY - 2009/1
Y1 - 2009/1
N2 - Through its intimate connection with the El Nĩo/Southern Oscillation system, climate variability in the tropical PacificOcean 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 records 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 climate. 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.
AB - Through its intimate connection with the El Nĩo/Southern Oscillation system, climate variability in the tropical PacificOcean 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 records 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 climate. 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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U2 - 10.1038/ngeo390
DO - 10.1038/ngeo390
M3 - Article
AN - SCOPUS:67649220594
SN - 1752-0894
VL - 2
SP - 46
EP - 50
JO - Nature Geoscience
JF - Nature Geoscience
IS - 1
ER -