The new coral data show that 20th century El Nino Southern Oscillation (ENSO) climate cycles are significantly stronger than ENSO variations captured in the fossil corals. But the data also reveal large natural variations in past ENSO strength, making it difficult to attribute the 20th century intensification of ENSO to rising carbon dioxide levels. Such large natural fluctuations in ENSO activity are also apparent in multi-century climate model simulations.
Photo: Roland Klein, Norwegian Cruise Lines
Georgia Tech researchers work underwater to remove cores from living coral colonies growing on Fanning Island in the central Pacific. In the laboratory, these “modern” cores provide records of the most recent period of climate changes for comparison to the fossil coral climate reconstructions.
“We looked at the long-term variability of ENSO in the climate models and asked how it compares to the long-term variability of ENSO in the real world,” said Kim Cobb, an associate professor in the School of Earth and Atmospheric Sciences at the Georgia Institute of Technology. “We show that they actually match fairly well. This project sets the stage for conducting more detailed data-model comparisons from specific time intervals to test the accuracy of ENSO characteristics in the various models.”
The research, sponsored by the National Science Foundation (NSF), was scheduled to be reported January 4 in the journal Science. Researchers from the Scripps Institution of Oceanography and the University of Minnesota also contributed to the work.
El Nino Southern Oscillation extremes drive changes in global temperature and precipitation patterns every two to seven years. The variations are particularly pronounced in the central tropical Pacific, where Cobb and her team collected the fossil corals used in this study. By analyzing the ratio of specific oxygen isotopes in the coral skeletons, the scientists obtained information about ENSO-related temperature and rainfall variations during the periods of time in which the corals grew.
“Fossil corals are the kings of El Nino reconstruction,” said Cobb. “Corals grow in the heart of the El Nino region, and with monthly-resolved records, they provide a very high level of detail.”
The researchers collected the coral samples by drilling into massive coral “rocks” rolled onto Pacific island beaches by the action of strong storms or tsunamis. Cobb and her team studied 17 such cores of varying lengths and ages recovered from beaches on Christmas and Fanning Islands, which are part of the Line Island chain located in the mid-Pacific.
The islands are ideal places for obtaining records of past ENSO activity because they are close enough to the source region for ENSO to be affected by its temperature and precipitation variations, but not so close that the islands’ corals are bleached by large temperature increases during strong El Nino warm events.
The study of each core began with careful dating, done by analyzing the ratio of uranium to thorium. That work was performed by co-authors Larry Edwards and Hai Cheng at the University of Minnesota. Once the age of each core was determined, Cobb and her team chose a subset of the collection to be studied in detail.
They sawed each core in half, then X-rayed the cross-sections to reveal the growth direction of each coral. The researchers then drilled out small samples of coral powder every millimeter down the core and analyzed them with mass spectrometers at Georgia Tech and the Scripps Institution of Oceanography to determine the ratio of oxygen isotopes.
The isotope ratio of the coral skeleton changes with the temperature and amount of rainfall, providing detailed information about environmental conditions during each period of the coral’s growth. As many as 20 samples are analyzed for each year of the coral’s lifetime.
“We are able to count back in time, following the seasonal cycles locked in the coral skeleton, as long as the core will allow us,” Cobb explained.
In all, Cobb’s team added 650 years of monthly-resolved information about ENSO variations across nearly 7,000 years. That required analyzing approximately 15,000 samples over the course of the study, which began in 2005.
Using the new sequences to quantify the range of natural variability in ENSO strength, the researchers have detected a modest, but statistically-significant increase in 20th century ENSO strength that may be related to anthropogenic climate change. However, the coral reconstruction shows an even higher level of ENSO strength 400 years ago, though its duration was shorter.
“The level of ENSO variability we see in the 20th century is not unprecedented,” Cobb said. “But the 20th century does stand out, statistically, as being higher than the fossil coral baseline.”
Information about the El Nino-Southern Oscillation is important for climate scientists because the cycle helps drive other aspects of global climate change.
“El Nino is something that people want to know about when they reconstruct past climate changes at a specific site,” Cobb said. “Our data will provide a reference for the magnitude of ENSO-related changes that may have occurred, and allow researchers to probe the causes of past climate changes evident in other paleoclimate records and in model simulations of past climates.”
The work has already called into question a long-held belief that ENSO was reduced some 6,000 years ago. Certain climate models support that picture, but Cobb said that fossil coral data from that period doesn’t support a reduction in ENSO strength.
Looking to future research, Cobb believes the work will be useful in helping scientists assess the accuracy of climate models.
“Prior to this publication, we had a smattering of coral records from this period of interest,” she said. “We now have tripled the amount of fossil coral data available to investigate these important questions. We have been able to provide a comprehensive view of recent variations in ENSO.”
Beyond the researchers already mentioned, the paper’s co-authors include Hussein R. Sayani and Emanuele Di Lorenzo from Georgia Tech and Christopher Charles, Niko Westphal and Jordan Watson from the Scripps Institution of Oceanography. In addition to the National Science Foundation, the project received assistance from Norwegian Cruise Lines, the National Geographic WAITT program, and the Palmyra Atoll Research Consortium.
The bulk of the research reported here was supported by the National Science Foundation (NSF) under Grant OCE-0752091. The content of this article is solely the responsibility of the authors and does not necessarily represent the official views of the NSF.Research News
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