The finding is the first physical evidence supporting what climate modelers have been predicting as the effects of global climate change on the subsurface ocean circulation.
The new study has been accepted for publication in Geophysical Research Letters, a journal of the American Geophysical Union.
"We're trying to find a way to understand how the warm water in the tropical Pacific has changed in the last century, but more importantly during the last several decades," says Branwen Williams, who conducted this research while a doctoral student at Ohio State University in Columbus, Ohio. She is now a postdoctoral fellow at the University of Toronto in Ontario, Canada.
"The Pacific is really important since it serves as a strong driver and changes in this ocean can have a very strong impact on global climate and oceanography."
What plagues modelers and researchers alike is the limited amount of information available about the ocean when studying climate change. Satellite data and physical measurements are mainly restricted to the ocean's surface waters. What happens deeper in the waters is often an unknown.
Williams and Andrea Grottoli, an associate professor of earth sciences at Ohio State and Williams' former advisor, turned to a prolific form of soft, flexible coral, the Gorgonians, growing on a reef off the island nation of Palau.
"These corals 'sway' with the current underwater," Grottoli explains, "like trees in the wind. Since they aren't restricted to shallow and warmer surface waters like other tropical corals, they provide an opportunity to reconstruct a picture of subsurface ocean circulation in a region."
Specifically, the researchers were interested in how the boundary layer between the warmer, shallow water and the colder deeper water -- the thermocline -- has changed. But directly measuring that over time and across a broad area is impossible.
Instead, they used the soft corals as a substitute, a proxy, for determining how the thermocline rose and fell over time. Working with samples taken from corals at five meters (16.4 feet), 85 meters (279 feet) and 105 meters (345 feet), they analyzed the chemical structure of the coral skeleton that had built up over time.
Slices cut through the base "trunk" of the coral revealed concentric circles resembling tree rings which showed the growth of the "trunk" over time. By analyzing material from the rings from the outer surface inward to the center, they assembled a growth record covering the last century or so.
They were looking for the ratio between two isotopes of nitrogen in the material as a clue to how the thermocline rose or fell over time. Warmer waters above the thermocline contained lower levels of nutrients resulting in organic matter with a high ratio of nitrogen-15 to nitrogen-14 isotopes. Waters below the thermocline held higher levels of nutrients resulting in organic matter with a low ratio of nitrogen-15 to nitrogen-14 isotopes.
As the polyps in the coral consumed the organic matter over the years, the nitrogen isotopes were chemically recorded in the coral. By comparing the nitrogen-15 to nitrogen-14 ratios in samples from the three depths, Williams and Grottoli were able to draw a picture of how the thermocline moved.
"Over several decades, specifically since the mid- to late-1970s, the records show that the mean depth of the thermocline has been getting shallower," Williams says.
The researchers did a similar analysis of the ratio of two carbon isotopes in the coral samples as well. "I think it's fair to say that the carbon isotope record supports this interpretation," Grottoli says. "It's another piece of evidence backing our conclusions."The researchers were also looking at how the coral record meshed with the Pacific Decadal Oscillation (PDO), a long-lived pattern of climate variability similar to the El Niño phenomenon.
While El Niño changes over a period of years, the PDO changes over decades.
"Climate modelers looking at how the Pacific might respond to global warming have predicted that the atmospheric patterns in the tropical Pacific would weaken, and if that happened, you would expect the thermocline to get shallower in the western tropical Pacific," Williams says.
"Our data are some of the first proxy data to support what the modelers have been predicting."
Grottoli saysthat the thermocline shift in the 1970s is important because it coincides with changes in the PDO from a negative phase to a positive phase.
"We think the thermocline rose when the PDO shifted," she says, "that it was a cumulative effect of both the natural variability of the PDO plus the warming global temperatures." Grottoli says that their coral record covered two other known times when the PDO shifted - in the 1920s and 1940s when average ocean termperatures were a bit lower than today - but neither caused a rise in the thermocline, based on their study.
The researchers want to repeat their study using coral samples from other locations, moving eastward across the Pacific, to test their findings that the thermocline shift wasn't a regional phenomenon, that it is occurring all across the ocean basin, Williams says.
Along with Williams and Grottoli, Patrick Colin, director of the Coral Reef Research Foundation, assisted in the project. Support for the research came from the National Science Foundation, the PADI Foundation, the Andrew Mellon Foundation and the National Ocean Sciences Accelerator Mass Spectrometry Facility at the Woods Hole Oceanographic Institution.Notes for Journalists
Or, you may order a copy of the paper by emailing your request to Maria-Jose Vinas at email@example.com. Please provide your name, the name of your publication, and your phone number.Images:
Contact information for the authors:
Branwen Williams, Tel. +1 (905) 828-5419; Mail firstname.lastname@example.org Andrea Grottoli, Tel +1 (614) 292-5782; Mail email@example.com
Maria-Jose Vinas | American Geophysical Union
Predicting unpredictability: Information theory offers new way to read ice cores
07.12.2016 | Santa Fe Institute
Sea ice hit record lows in November
07.12.2016 | University of Colorado at Boulder
In recent years, lasers with ultrashort pulses (USP) down to the femtosecond range have become established on an industrial scale. They could advance some applications with the much-lauded “cold ablation” – if that meant they would then achieve more throughput. A new generation of process engineering that will address this issue in particular will be discussed at the “4th UKP Workshop – Ultrafast Laser Technology” in April 2017.
Even back in the 1990s, scientists were comparing materials processing with nanosecond, picosecond and femtosesecond pulses. The result was surprising:...
Have you ever wondered how you see the world? Vision is about photons of light, which are packets of energy, interacting with the atoms or molecules in what...
A multi-institutional research collaboration has created a novel approach for fabricating three-dimensional micro-optics through the shape-defined formation of porous silicon (PSi), with broad impacts in integrated optoelectronics, imaging, and photovoltaics.
Working with colleagues at Stanford and The Dow Chemical Company, researchers at the University of Illinois at Urbana-Champaign fabricated 3-D birefringent...
In experiments with magnetic atoms conducted at extremely low temperatures, scientists have demonstrated a unique phase of matter: The atoms form a new type of quantum liquid or quantum droplet state. These so called quantum droplets may preserve their form in absence of external confinement because of quantum effects. The joint team of experimental physicists from Innsbruck and theoretical physicists from Hannover report on their findings in the journal Physical Review X.
“Our Quantum droplets are in the gas phase but they still drop like a rock,” explains experimental physicist Francesca Ferlaino when talking about the...
The Max Planck Institute for Physics (MPP) is opening up a new research field. A workshop from November 21 - 22, 2016 will mark the start of activities for an innovative axion experiment. Axions are still only purely hypothetical particles. Their detection could solve two fundamental problems in particle physics: What dark matter consists of and why it has not yet been possible to directly observe a CP violation for the strong interaction.
The “MADMAX” project is the MPP’s commitment to axion research. Axions are so far only a theoretical prediction and are difficult to detect: on the one hand,...
16.11.2016 | Event News
01.11.2016 | Event News
14.10.2016 | Event News
07.12.2016 | Health and Medicine
07.12.2016 | Life Sciences
07.12.2016 | Health and Medicine