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Will the Ocean Circulation Be Unbroken?Line W moorings monitor an intersection where key climate-influencing currents converge |
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| Enlarge ImageLine W is an array of five moorings that has been monitoring changes in two currents that play important roles in regulating Earth's climate: the Gulf Stream (orange area) and the Deep Western Boundary Current hugging the U.S. Eastern Seaboard (enlarge for details). |
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| Enlarge ImageLine W monitors a key junction in the ocean's global circulation (enlarge for details). (E. Paul Oberlander, Woods Hole Oceanographic Institution) |
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| Enlarge ImageLine W monitors the southward, cold Deep Western Boundary Current and the northward, warm, surface Gulf Stream (enlarge for details). (E. Paul Oberlander, Woods Hole Oceanographic Institution) |
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| Enlarge ImageResearchers prepare to launch a profiler, which will travel up and down a mooring cable every five days, measuring seawater properties. (Jim Canavan, Woods Hole Oceanographic Institution) |
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| WHOI physical oceanographer John Toole (Patrick Rowe, Woods Hole Oceanographic Institution) |
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If the world’s climate is going to change, we will see signs in the ocean.
The atmosphere and oceans are intricately linked; nowhere is that
better demonstrated than in the North Atlantic Ocean, where current
systems carry great volumes of warm and cold water into and out of the
region, creating a critical turnaround point in the global circulation
of the oceans.
In the tropical Atlantic, intense sunlight warms the ocean, while dry
trade winds cause surface waters to evaporate and become saltier. The
Gulf Stream carries this warm, salty water north along the U.S. East
Coast and then toward Europe, before it transitions into the North
Atlantic Current and heads north. As this water reaches higher
latitudes, it releases heat to the atmosphere, tempering winters in the
North Atlantic region and leaving behind saltier, cooler, and denser
waters.
These transformed waters sink to the depths and form the Deep Western
Boundary Current, which flows southward along the East Coastbeneath
the northward-flowing Gulf Streamand into the South Atlantic. This
process of sinking and southward flow draws more warm water northward
to replace it and contributes to a worldwide circulation pattern
sometimes referred to as the Ocean Conveyor.
For decades, scientists have sampled these currents to gain a fuller
understanding of the North Atlantic’s critical role in influencing
regional and global climate. But they have been limited by their
inability to get more than point measurementsthat is, observations in
one geographic place at one moment in time (a day, or maybe a month,
but rarely longer).
To help remedy that situation, Woods Hole Oceanographic Institution
researchers established a long-term observing system on the continental
slope south of New England, where the Gulf Stream and Deep Western
Boundary Current align roughly like an artery and vein in the Atlantic
Ocean circulation system. Combining an array of moored instruments with
shipboard observations, the "Line W" program has been directly
measuring the properties and variations of these two currents between
Cape Cod and Bermuda.
Continuous, long-term observations
Line W is named for Valentine Worthington, the late WHOI physical
oceanographer who devoted a considerable part of his career to
measuring and understanding the system of currents in the North Atlantic.
Building on the work of Worthington and other pioneers, WHOI physical
oceanographers John Toole, Terry Joyce, Ruth Curry, and Bob Pickart, as
well as Lamont-Doherty Earth Observatory geochemist Bill Smethie, are
working to chronicle variations in the Deep Western Boundary Current
and Gulf Stream.
Does the volume of water in the current change from year to year? Is
the water growing warmer or cooler, fresher or saltier? And what are
the consequences of such changes for the exchange of heat and moisture
with the atmosphere and for the circulation of the entire Atlantic?
In the 1950s, researchers from WHOI and the Bermuda Biological Station
for Research began a long time-series of water measurements at Station
S, about 15 miles off the coast of Bermuda. Every two weeks since June
1954, researchers have returned to that spot in the middle of the
Sargasso Sea and measured the water properties from the surface to the
depths. That long-term data set has proved invaluable for giving broad
views of the Gulf Stream, the layering (or “stratification”) of the
ocean over time, and other aspects of Atlantic circulation.
Following the Station S model, WHOI scientists launched the Line W
effort in October 2001 with the placement of a single mooring about 320
kilometers (200 miles) southeast of Cape Cod at 39°N 69°W. That
initial effort, funded by the G. Unger Vetlesen Foundation, was called
Station W. In 2003, having proved the value of the concept to the
National Science Foundation, the researchers secured funding to add
four additional moorings and to make twice-yearly ship-based
observations in the area over four years.
Measurements over time and space
The Line W array was installed in April 2004. Three of the five
moorings in the array support “moored profilers,” which crawl up and
down a steel mooring cable, carrying sensors that continuously measure the
temperature, salinity, and velocity of water from the surface to the
seafloor, storing the data in computer memory. The other two moorings
have individual sensors distributed in the water column to take
long-term measurements at key points.
The Line W array records the velocity and layering of the Deep Western
Boundary Current, while also documenting the intensity of the Gulf
Stream as it meanders. By design, the array lies directly beneath the
track of the Jason ocean-observing satellite, which measures features
of the sea surface over Line W every 10 days, complementing the
underwater measurements.
Line W is one component in a long-term, international effort to observe
most of the critical regions of the North Atlantic circulation system.
In particular, it is linked closely to the United Kingdom’s RAPID
Climate Change Programme, which has set a line of moorings northeast of
Line W and another along a line stretching from Florida to North Africa
at 26°N.
WHOI physical oceanographer Michael McCartney recently established a
separate but complementary mooring, positioned in the middle of the
Gulf Stream and along the same satellite track as Line W and the
venerable Station S. The Gulf Stream Transport Observations mooring, or
GUSTO, is a hardy conventional mooring designed to measure changes in
the strength and structure of the Gulf Stream over time.
The new mooring is actually the second incarnation of GUSTO. A previous
version was developed and deployed in 1982 by McCartney and former WHOI
physical oceanographers Harry Bryden, Dale Haidvogle, and Val
Worthington. By combining data from the original GUSTO mooring,
analyzed by former MIT/WHOI Joint Program student Mindy Hall, with
those from the new GUSTO mooringas well as observations from another
Gulf Stream measurement program of the late 1980s (known as
SYNOP)oceanographers will paint a clearer picture of changes over the
decades in the Gulf Stream.
Gauging the ocean’s pulse
With three years in the water and one more to go, the Line W program
has been amassing mountains of data about the day-by-day and
season-by-season characteristics of currents flowing through the
northwestern Atlantic.
So far, the research team has observed interesting changes in waters at
intermediate depth in the North Atlantic. These appear to relate to
changes in the amount of dense, cold waters that scientists have
observed sinking upstream in the Labrador Sea. The team also sees
that since 2000, there has been decreasing salinity in the densest waters of the Deep Western Boundary
Current at Line Wa signal, they believe, of fresher
upstream waters spilling over the Greenland-Scotland Ridge into the
North Atlantic from the Greenland, Iceland, and Norwegian Seas (see
“Interrogating the Ocean Conveyor” and “Fresher Ocean, Cooler Climate").
Ultimately, integrating Line W data with other observing programs will
advance understanding of how changes in the waters of the northern
North Atlantic Ocean are propagated to lower latitudes, and vice
versa, and how these changes affect the rest of the global ocean
circulation.
Researchers often point to changes at the poles as the proverbial
“canary in a coal mine,” providing warning of global change. But the message could well be delivered by variations in the North
Atlantic Ocean’s circulation, which should come through
loud and clear at Line W.
Line W and Station W were made
possible through the support of the G. Unger Vetlesen Foundation, the
WHOI Ocean and Climate Change Institute, and the National Science
Foundation. Line W collaborators include John Smith of the Bedford
Institute of Oceanography, as well as scientists from the United
Kingdom’s RAPID Climate Program, particularly Chris Hughes, Ric
Williams, and David Marshall.

To Follow the WaterFrom a new book by Dallas MurphyIn April 2005, author Dallas Murphy accompanied an expedition aboard the research vessel Oceanus to recover and redeploy moorings at Line W and wrote about it in a chapter of his new book, To Follow the Water: Exploring the Ocean to Discover Climate from the Gulf Stream to the Blue Beyond. Here is an excerpt:
Shortly after lunch, word came down from the bridge: “Ten minutes from
station.” Oceanus slowed gradually to a stop, and her motion,
boisterous underway, turned nasty in the messy sea state. We moved as
though moving were new to us, from handhold to handhold. The air seemed
cooler now, and the low clouds glowered. The fantail, built low to the
water on research vessels to facilitate deploying and retrieving heavy
objects, was almost constantly awash. The technicians (called
“sci-techs” aboard this vessel) and deck crew, led by bosun Jeff Stolp,
were gearing up and getting ready to pull the Profiler back into human
possession. The winch operation was in his place, and Stolp signaled
him to run out the steel A-frame structure mounted above the stern. I
was feeling a bit confused from that hit of Dramamine and the raw
unfamiliarity of it all, and maybe that was why I didn’t understand how
they were going to retrieve the thing. There was nothing on the
surface. To keep it safe from passing ships the mooring ball is fixed
some fifty meters beneath the surface. I didn’t want to interrupt the
flurry of activity with remedial questions, so I settled for
unobtrusive eavesdropping. Spotting John Toole and Scott Worrilow,
chief sci-tech, standing by a computer terminal at the after end of the
lab, I staggered that way to peer over their shoulders.
“It's an acoustic release,” Scott offered. “There are two releases for
redundancy. They’re mounted at the bottom of the cable near the anchor.
We just pinged them, told them to wake up. Hear those pings? Every ten
seconds. That’s the signal from the releases saying, ‘We’re awake and
ready for instructions.’ ” Scott keyed in their coded instructions,
then he and John waited silently for confirmation. “Done. It’s coming
up. It’ll be away on the starboard side.” We went topside to look for
it.
The big orange float popped to the surface away to starboard, just
where it was supposed to be. Captain (Larry) Bearse deftly laid Oceanus
alongside and held her there bow-on to the stiff wind. Bosun Stolp
ordered the boom arm on the crane run out, someone got a line through
the lifting ring on the float, and Stolp signaled the winch driver to
take up. He called for a halt when the ball had risen above the rail,
and the deck crew hustled to get lines on it to arrest its swinging. No
words were needed. Everyone working together in sync with the
thirty-degree rolls, Jeff signaled the winch driver to bring it inboard
and lower it onto its dedicated rack, like a giant golf-ball tee, and
then everyone relaxed. I felt like applauding, but this was just
business as usual for these guys. The sci-techs unshackled the float,
then led the wire to another winch bolted on the fantail. Stolp snapped
his fingers against his palm, the universal “take-it-up” signal, and
the winch driver, standing behind a metal-mesh screen for protection
should the cable snap, engaged the four-foot diameter drum, and the
retrieval process began. It took more than two hours to complete, and
this was the shallowest of five moorings. One would not expect
lubberliness aboard Oceanus, but I was filled with admiration that day
and every other for the impeccable seamanship on the bridge and on deck.
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Posted: October 31, 2007 [top] |
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