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May 11, 2017
Contact: Shelley Dawicki

Marine Species Distribution Shifts Will Continue Under Ocean Warming

lobster

Changes impact local fishing communities, resource management

Scientists using a high-resolution global climate model and historical observations of species distributions on the Northeast U.S. Shelf have found that commercially important species will continue to shift their distribution as ocean waters warm two to three times faster than the global average through the end of this century. Projected increases in surface to bottom waters of  6.6 to 9 degrees F (3.7 to 5.0 degrees Celsius) from current conditions are expected.

The findings, reported in Progress in Oceanography, suggest ocean temperature will continue to play a major role in where commercially important species will find suitable habitat. Sea surface temperatures in the Gulf of Maine have warmed faster than 99 percent of the global ocean over the past decade.  Northward shifts of many species are already happening, with major changes expected in the complex of species occurring in different regions on the shelf, and shifts from one management jurisdiction to another. These changes will directly affect fishing communities, as species now landed at those ports move out of range, and new species move in.

“Species that are currently found in the Mid-Atlantic Bight and on Georges Bank may have enough suitable habitat in the future because they can shift northward as temperatures  increase,”  said lead author Kristin Kleisner, formerly of the Northeast Fisheries Science Center (NEFSC)‘s Ecosystems Dynamics and Assessment Branch and now a senior scientist at the Environmental Defense Fund. ”Species concentrated in the Gulf of Maine, where species have shifted to deeper water rather than northward, may be more likely to experience a significant decline in suitable habitat and move out of the region altogether.”


Projected thermal habitat for American lobster in the fall (top image) and spring (bottom image). These animations show projected distributions of suitable thermal habitat based on the NOAA Geophysical Fluid Dynamics Laboratory's high-resolution global climate model (CM2.6). In the 80-year model run, atmospheric CO2 increases by 1% per year and doubles by year 70. This results in a global surface warming of 2°C (3.6°F), which is equivalent to the 2060-80 time period in the IPCC's RCP8.5 (highest emissions scenario). Therefore, the time steps (60-80) correspond roughly to the years 2060-80 in the IPCC’s RCP8.5 emissions scenario. It is important to note that these are ONLY projections of thermal habitat and DO NOT include other important factors such as fishing mortality, species interactions, and bottom-up forcing.

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The researchers used bottom trawl survey data collected between 1968 and 2013 on the shelf to estimate niches for 58 demersal and pelagic species.  A high-resolution global climate model known as CM2.6, developed by the NOAA Geophysical Fluid Dynamics Laboratory (GFDL) in Princeton, New Jersey, was used to generate projections of future surface and bottom ocean temperatures across the region. The future temperatures were then used to project where marine species would find suitable habitat.

“Similar studies in the past used a coarse model with a roughly 100-kilometer or 62-mile ocean resolution, while the new model has a 10-kilometer or 6.2-mile ocean resolution, making the simulation of oceanic and atmospheric features much more accurate,“ said Vincent Saba of the NEFSC‘s Ecosystems Dynamics and Assessment Branch, who works at GFDL and is a co-author of the study.

Saba has compared the difference between the coarse model and the new high-resolution model as being similar to the difference between an old standard definition television set and today’s ultra high definition screens.

Researchers looked at species distributions in spring and fall in the Gulf of Maine on the northern part of the Northeast Shelf and those on the southern end, from Georges Bank to the Mid-Atlantic Bight. They also examined what the shifting distributions might mean for fishing communities by looking at the current and potential future distance between the main fishing port in each state and the center of the distribution of suitable thermal area for the top-landed species by weight in each state.

Key northern species including Acadian redfish, American plaice, Atlantic cod, haddock, and thorny skate may lose thermal habitat, while spiny dogfish and American lobster may gain. Projected ocean warming in the Gulf of Maine may create beneficial conditions for American lobster populations, and they may continue to be accessible to fishing ports in the region.

In contrast, species like monkfish, witch flounder, white hake and sea scallops may remain accessible to major local fishing ports but could experience strong declines in habitat due to ocean warming.  Atlantic cod, which is at the southern end of its range, may find suitable thermal habitat off the shelf entirely or in more northern waters in Canada.

In states south of New York, the distance to the centers of species distribution from ports may increase for some species, including summer flounder, which is currently the third most-landed species in Virginia. In North Carolina, the distance from ports to the center of distribution may increase for all six of the top landed species. Among the top six species landed in Virginia, only Atlantic croaker and striped bass are projected to have more suitable habitat.

“Warming waters may have a positive effect on smooth dogfish, Atlantic croaker, and striped bass  in the southern part of the Northeast Shelf, with increases in suitable habitat in terms of area and species abundance, “ Kleisner said. “But these species are also shifting northward and the bulk of the biomass of some species may be further from the main ports in southern states, making it more costly for fishermen to access these species. Conversely, as species move into new regions, fishermen may have new opportunities.”

The projections indicate that as species shift from one management jurisdiction to another, or span state and federal jurisdictions, increased collaboration among management groups will be needed to set quotas and establish allocations.

“These changes will depend on the pace of climate change and on the ability of species to adapt or shift elsewhere to maintain a preferred habitat,” said Kleisner.  “We did not examine fishing pressure, species interactions and other factors that may influence future distributions. However, given the historical changes observed on the Northeast Shelf over the past five decades and confidence in the projection of continued ocean warming in the region, it is likely there will be major changes within this ecosystem.”

“Those changes will result in ecological, economic, social, and natural resource management challenges throughout the region,” Kleisner said. “It is important to understand large-scale patterns in these changes so that we can plan for and mitigate adverse effects as much as possible.”

Funding for this joint project between NOAA’s Northeast Fisheries Science Center and The Nature Conservancy study was provided by a grant from the Gordon and Betty Moore Foundation.

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The Northeast Fisheries Science Center conducts ecosystem-based science supporting stewardship of living marine resources under changing climatic conditions. Follow us on Facebook and Twitter.

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