“2024 global sea surface and air temperatures exceeded 2023
as the warmest year on record, but colder than average temperatures were
observed in the Northeast U.S. Oceanographic
and ecological conditions in the Northwest Atlantic were markedly different in
2024 compared to recent years.
“…Late 2023 and early 2024 observations indicate movement of
cooler and fresher water into the Northwest Atlantic, although there are
seasonal and local exceptions to this pattern.
Anomalously cold and low salinity conditions were recorded throughout
the Northeast Shelf and were widespread across the Slope Sea for much of the year. These cooler and fresher conditions are
linked to the southward movement of the eastern portion of the Gulf Stream and
possibly an increased influx of Labrador Slope and Scotian Shelf water into the
system.”
The cooler, fresher water wasn’t limited to the Gulf of
Maine. In February 2024, sea surface
temperatures along the outer continental shelf were between 2.5 and 5 degrees
Centigrade lower than the average February temperature for the
years 2000 through 2020, even though waters closer inshore somewhat exceeded
the long-term average temperature. The
NMFS publication stated that
“Colder, fresher water detected deep in the Jordan Basin
[region of the Gulf of Maine] for the first half of 2024 suggests and influx of
Labrador Slope and Scotian Shelf water, which resulted in colder and fresher
conditions throughout the Northwest Atlantic and contributed to the increased
size and colder temperatures of the Mid-Atlantic Cold Pool.”
A
recent, related NMFS news release said that
“Researchers expect the Gulf of Maine to be 0.9 to 1.8
degrees Fahrenheit (0.5 to 1 degree Celsius) cooler this summer [of 2025]
compared to the average summer temperature…
“A companion longer-term outlook, also developed by NOAA
scientists, suggests that more frequent inflows of cooler deep water may
continue to temper warming in the basin for the next several years.”
The 2005 State of the Ecosystem report reveals that
“the center of distribution for a suite of 48 commercially or
ecologically important fish species along the entire Northeast Shelf continues
to show movement toward the northeast and generally into deeper water. Habitat model-based species richness suggest shifts
of both cooler and warmer water species to the northeast.”
However, since it also notes that
“Long-term oceanographic projections forecast a temporary
pause in warming over the next decade due to internal variability in
circulation and a southward shift of the Gulf Stream,”
it is reasonable to ask whether the current cooling trend
will interrupt the northeastward shift in fish stocks, and how fish stocks will
react to the cooling water.
The recent NMFS release provides some insight, stating that
“Bottom-water temperatures influence the productivity of
groundfish, like cod, haddock, pollock, and several species of flounder, which
prefer cooler water. Lobster, the most
valuable fishery in the northeast, are also temperature-sensitive. Warming waters along the New England coast in
recent decades have contributed to the collapse of the southern New England
lobster population while the Gulf of Maine population has boomed. Researchers expect that cooler waters will
impact this economically and culturally important species.”
Given that the cooler water extends into the Mid-Atlantic,
it’s hard not to wonder whether anyone might be regretting the Atlantic States
Marine Fisheries Commission’s American Lobster Management Board’s decision not
to adopt a
moratorium on harvest of the southern New England lobster stock, as recommended
by the American Lobster Technical Committee in 2010. At the time, the Technical Committee only
recommended a 5-year-long moratorium, but observed that
“Environmental changes, most notably temperature, likely have
forced lobster to seek more suitable habitat in deeper water. Larvae produced by displaced lobster may be
lost to traditional inshore nursery grounds.
The fishery has adapted to the changes in the resource by shifting
effort further offshore. However,
fishing continues in most inshore portions of [southern New England], and
continued harvest represents lost spawning stock.
“A moratorium provides the maximum likelihood to rebuild the
stock to a level that can support a sustainable fishery. Rebuilding the currently depleted [southern
New England] stock may take longer than five years. Cady and Agnew (2004) reviewed stock
recoveries of depleted marine resources and reported that invertebrate
fisheries most likely to recover were those with reductions in predator
pressure, in the center of their geographic range and under favorable
regimes. They that the predicted length
of recoveries should be treated with caution and conclude that a few stocks
have recovered within a decade, but that most require longer.”
Such a moratorium, if sustained until the stock showed strong signs of recovery, would have maximized the number of breeding-age adults that might have been able to take advantage of the current cooling trend, and might have been able to take advantage of the cooler waters to increase lobster recruitment. However, that opportunity was lost a long time ago. The southern New England lobster stock is now at the lowest level of abundance ever recorded, and continues to decline.
However, the cooling may come soon enough to bail out the
lobster fishery in
the Gulf of Maine, where fishermen who failed to learn any lessons from the collapse of the
southern New England stock, adamantly opposed modest restrictions intended to
prevent a similar decline off northern New England, and caused the American
Lobster Management Board to back off from imposing such restrictions in the
Gulf of Maine and off eastern Cape Cod.
It is very possible that the cooling water will reverse a trend of
declining lobster recruitment in the region, and that lobstermen will feel
vindicated in successfully opposing science-based management—at least until the
cooling trend reverses, and increasing water temperatures drive Gulf of Maine lobster
recruitment down once again.
But the most interesting question may be how the cooler and
less saline waters flowing along the outer continental shelf will impact the
black sea bass population.
The ASMFC’s Summer Flounder, Scup, and Black Sea Bass
Management Board, which is not required to follow the Scientific and
Statistical Committee’s advice, agreed with the dissenters on the Monitoring
Committee and refused to reduce black sea bass catch limits. The Mid-Atlantic Council, which was bound to
follow the SSC’s guidance, did cut landings by 20 percent, creating a rift
between federal and state management measures, that NMFS—which also claims not
to be bound by the SSC’s decisions—resolved by ignoring the Council advice and extending
the ASMFC decision into federal waters.
It was a strange debate and an even stranger resolution, but
now we have to ask whether the Scientific and Statistical Committee was really
right all along.
That’s
because black sea bass recruitment—the number of young fish that enter the
population each year—is not primarily driven by the size or the spawning stock
or by the number of juvenile fish that are produced. Instead, recruitment is driven by the
oceanographic conditions that the first-winter fish experience when they spend
that first winter at or near the edge of the continental shelf. Warmer, more saline water typically results
in strong black sea bass recruitment. The
very strong 2011 year class, which was most prevalent north of Hudson Canyon,
can probably be attributed to such favorable conditions, as the 2025
State of the Ecosystem report revealed that
“2012 had among the warmest surface and bottom temperatures
in New England. A large proportion of
the Georges Bank and Mid-Atlantic regions had bottom temperatures above the 15oC
thermal tolerance for most groundfish, with some days in the Mid-Atlantic
exceeding the 24oC potential mortality limit.”
Now, with cooler, less saline water expected to prevail for “several
years,” there is good reason to believe that the 2024 stock assessment’s predictions
of lower black sea bass recruitment may have been right on target, if not,
perhaps, a little optimistic, and also to believe that the current regulations, which failed to
follow the Scientific and Statistical Committee’s advice and allowed higher
harvest than the SSC recommended, may have left the black sea bass stock more
vulnerable to the predicted change in ocean conditions.
We can only wait and watch how the situation plays out, to
learn how long the cooler, fresher water maintains its presence off New England
and the Mid-Atlantic, and also to learn how that presence will affect the current
and future abundance of various speces.
But as is always the case when changing ocean conditions add
to the uncertainty in managing fish stocks, managers should definitely practice precaution when setting management measures.
A 16.5 in recreational size limit for sea bass in NYS is still ridiculously to large.
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