Accelerated warming of the continental shelf off U.S. Northeast Coast – ‘The warming rate since 2002 is 15 times faster than from the previous 100 years’Posted by Jim at Friday, June 19, 2015
11 June 2015 (WHOI) – A couple of unexplained large scale changes in the waters off the northeast coast of the U.S. have oceanographers perplexed: an accelerated rate of sea level rise compared to most other parts of the world; and the disturbing signs of collapsing fisheries in the region.
A new study by physical oceanographers at Woods Hole Oceanographic Institution (WHOI), published in the Journal of Geophysical Research, shows that water temperatures in this continental shelf region have been trending upward, with unprecedented warming occurring over the last 13 years. The study also suggests a connection between sea level anomalies and water temperature along the continental shelf.
“The warming rate since 2002 is 15 times faster than from the previous 100 years,” says co-author Glen Gawarkiewicz, a WHOI senior scientist. “There's just been this incredible acceleration to the warming, and we don't know if its decadal variability, or if this trend will continue.”
The scientists compared their findings with a study of surface waters using data collected by Nantucket Light ship, and other light ships up and down the East Coast between 1880 and 2004, previously analyzed by Steve Lentz of WHOI and Kipp Shearman of Oregon State University. The new study shows that recent accelerated warming is not confined to the surface waters, but extends throughout the water column.
“Others have reported on the temperature increase in this region,” says Gawarkiewicz’s colleague, WHOI assistant scientist Magdalena Andres, “but they've been confined to looking at the surface temperatures from satellites or buoys.” And Gawarkiewicz and Andres wanted to understand how deep the warming went.
The research is based upon a rare collection of temperature data from the waters off the northeast coast of the U.S. that were collected in collaborative effort between scientists and the operators of the container ship Oleander, which routinely travels between Bermuda and New Jersey. The effort, which began in the late 1970s with funding from NOAA/NMFS, involved launching bathythermographs along the ship’s track to collect temperature data approximately 14 times each year. Later the program was funded through the National Science Foundation and the University of Rhode Island and Stony Brook University. The bulk of the prior analysis has been on velocity data also collected by the Oleander.
“The Oleander data is special, because it goes through the whole water column on the shelf. And if you're a fish living on the bottom, you care more about that,” says Andres. “It was this trove of shelf temperature data that we could use to help us address these questions.”
That’s where Jacob Forsyth, lead author of the study, came into the picture. In 2014, Forsyth had just begun an 11-week summer student fellowship at WHOI, with Andres and Gawarkiewicz as his co-advisors. “On a lark, we had Jacob look at the data, not knowing if it would pan out,” says Andres. “But it was a super data set, and Jacob did a great job analyzing the data,” she added.
A physics and economics major at Bowdoin College, Forsyth had taken just one college oceanography course but had a passion for the ocean and for science. Early into his fellowship, Forsyth found himself at WHOI immersed in the academic literature, quality controlling nearly 40 years’ worth of data, and teaching himself MatLab to begin looking at this database no one had really assembled before.
The bulk of the data were collected by volunteer observers who rode the Oleander from New Jersey to Bermuda at monthly intervals deploying the bathythermographs, a probe that is dropped from a ship to measure the temperature as it falls through the water. Two very small wires transmit the temperature data to the ship where it is recorded for later analysis. Because water temperature can vary by layer, it was important to obtain information on the temperature structure of the ocean to depths of up to 700 meters. More recently an automated data collection system has been used which was developed by Dave Fratantoni, formerly of WHOI.
The researchers looked at the temperatures for a given year and averaged them across the shelf, to get a temperature index for the year. Their work showed that temperature has been steadily increasing, and most recently, it's been getting warmer, faster. Superimposed on that, they found a lot of year-to-year variability.
Andres says, “what's controlling the trends may be different than what's controlling the year-to-year changes.” She notes, “There are two questions: What are the mechanisms for the slow, sustained warming? And what is it for the inter-annual variability? Those don't have to be the same thing.”
What the researchers did determine is that the slow, sustained warming is not just due to warming of the atmosphere, but that it's something related to dynamics of the shelf break, where the shallow continental shelf abuts the deeper continental slope.
“The warming more recently seems to be at the edge of the continental shelf, which would indicate there might be a Gulf Stream role or a slope water role in the warming,” says Gawarkiewicz, “and that's different than if it was all from the atmosphere over the last 12 years, because that would be uniform and near the surface.” Investigating the exact cause is among their next steps.
In addition to analyzing the warming trend, Forsyth, who will enter the MIT-WHOI Joint Program in Oceanography this summer, used the data to search for a relationship between sea levels and temperatures. He found, in fact, there is a very strong relationship between the two, where sea level anomalies may serve as a predictor of shelf temperature. Forsyth determined the lag between the two indicators was approximately two years – enough time to give environmental monitors a chance to respond.
The researchers underscore the importance of a long, continuous set of measurements, and that they are hard to come by due to the limitations of funding. The Oleander program and the newly installed Pioneer Array, a part of a larger NSF-funded network of observatories in the Atlantic and Pacific called the Ocean Observatories Initiative, which is positioned along the shelf break, will collect continuous measurements, so critical in understanding the dynamics of the region. Because it’s a productive fishing ground, the warming at lower depths can have a big impact on the distribution and abundance of fish in the area.
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ABSTRACT: Expendable bathythermographs (XBTs) have been launched along a repeat track from New Jersey to Bermuda from the CMV Oleander through the NOAA/NEFSC Ship of Opportunity Program about 14 times per year since 1977. The XBT temperatures on the Middle Atlantic Bight shelf are binned with 10 km horizontal and 5 m vertical resolution to produce monthly, seasonally, and annually averaged cross-shelf temperature sections. The depth-averaged shelf temperature, Ts, calculated from annually averaged sections that are spatially averaged across the shelf, increases at 0.026 ± 0.001°C yr−1 from 1977 to 2013, with the recent trend substantially larger than the overall 37 year trend (0.11 ± 0.02°C yr−1 since 2002). The Oleander temperature sections suggest that the recent acceleration in warming on the shelf is not confined to the surface, but occurs throughout the water column with some contribution from interactions between the shelf and the adjacent Slope Sea reflected in cross-shelf motions of the shelfbreak front. The local warming on the shelf cannot explain the region's amplified rate of sea level rise relative to the global mean. Additionally, Ts exhibits significant interannual variability with the warmest anomalies increasing in intensity over the 37 year record even as the cold anomalies remain relatively uniform throughout the record. Ts anomalies are not correlated with annually averaged coastal sea level anomalies at zero lag. However, positive correlation is found between 2 year lagged Ts anomalies and coastal sea level anomalies, suggesting that the region's sea level anomalies may serve as a predictor of shelf temperature.