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WHOI to Launch New Center for Ocean and Climate Research

Today WHOI announced the establishment of the Francis E. Fowler IV Center for Ocean and Climate to seek new knowledge and solutions at the intersection of oceanography and climate science. A generous gift from Francis E. Fowler, IV established the center and will enable it to immediately commence operations.

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Study Finds No Direct Link Between North Atlantic Ocean Currents, Sea Level Along New England Coast

A new study by the Woods Hole Oceanographic Institution (WHOI) clarifies what influence major currents in the North Atlantic have on sea level along the northeastern United States. The study, published June 13 in the journal Geophysical Research Letters, examined both the strength of the Atlantic Meridional Overturning Circulation (AMOC)—a conveyor belt of currents that move warmer waters north and cooler waters south in the Atlantic—and historical records of sea level in coastal New England.

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WHOI, Falmouth Win Second Seaport Economic Council Grant

The Iselin Marine Facility, shown here in 1960, was constructed in its current configuration in 1969 to accommodate an expanding fleet. © Woods Hole Oceanographic Institution

Members of the Massachusetts Seaport Economic Council (SEC) gave the green-light to a $1 million grant proposal from the Town of Falmouth and Woods Hole Oceanographic Institution (WHOI). The SEC, chaired by Lieutenant Governor Karyn Polito, promotes economic growth in the maritime sector through competitive grants to municipalities and their partners.

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Study Finds Link Between River Outflow and Coastal Sea Level

Study Finds Link Between River Outflow and Coastal Sea Level

Sea levels in coastal areas can be affected by a number of factors: tides, winds, waves, and even barometric pressure all play a role in the ebb and flow of the ocean. For the first time, however, a new study led by the Woods Hole Oceanographic Institution (WHOI) has shown that river outflow could play a role in sea level change as well.

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Fueling a Deep-Sea Ecosystem

Fueling a Deep-Sea Ecosystem

Miles beneath the ocean surface in the dark abyss, vast communities of subseafloor microbes at deep-sea hot springs are converting chemicals into energy that allows deep-sea life to survive, and even thrive, in a world without sunlight. Until now, however, measuring the productivity of subseafloor microbe communities (or how fast they oxidize chemicals and the amount of carbon they produce) has been nearly impossible.

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Galapagos Expedition Reveals Unknown Seamounts, New Species

Galapagos Expedition Reveals Unknown Seamounts, New Species

During a three-week expedition in August, an international team led by the Woods Hole Oceanographic Institution (WHOI), in partnership with the Charles Darwin Foundation for the Galápagos Islands and in close collaboration with the Galápagos National Park Directorate, conducted the first scientific expedition to map and characterize the seamounts on the Galápagos platform and the diverse marine life that these underwater mountains support.

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River Buries Permafrost Carbon at Sea

As temperatures rise, some of the carbon dioxide stored in Arctic permafrost meets an unexpected fate—burial at sea. As many as 2.2 million metric tons of carbon dioxide (CO2) per year are swept along by a single river system into Arctic Ocean sediment, according to a new study led by Woods Hole Oceanographic Institution (WHOI) researchers and published today in Nature. This process locks away the greenhouse gas and helps stabilize the earth’s CO2 levels over time, and it may help scientists better predict how natural carbon cycles will interplay with the surge of CO2 emissions due to human activities.

“The erosion of permafrost carbon is very significant,” says WHOI Associate Scientist Valier Galy, a co-author of the study. “Over thousands of years, this process is sequestering CO2 away from the atmosphere in a way that amounts to fairly large carbon stocks. If we can understand how this process works, we can predict how it will respond as the climate changes.”

Permafrost—the permanently frozen ground found in the Arctic and Antarctic and in some alpine regions—is known to hold billions of tons of organic material, including vast stores of CO2. Amid concerns about rising Arctic temperatures and their impact on permafrost, many researchers have directed their efforts to studying the permafrost carbon cycle—the processes through which the carbon circulates between the atmosphere, the soil and surface (the biosphere), and the sea. Yet how this cycle works and how it responds to the warming, changing climate remains poorly understood.

Galy and his colleagues from Durham University, the Institut de Physique du Globe de Paris, the NERC Radiocarbon Facility, Stockholm University, and the Universite Paris-Sud set out to characterize the carbon cycle in one particular piece of the Arctic landscape—northern Canada’s Mackenzie River, the largest river flowing into the Arctic Ocean from North America and that ocean’s greatest source of sediment. The researchers hypothesized that the Mackenzie’s muddy water might erode thawing permafrost along its path and wash that biosphere-derived material and the CO2 within it into the ocean, preventing the release of that CO2 into the atmosphere.

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Tracking Fish Through a Coral Reef Seascape

Ocean scientists have long known that juvenile coral reef fishes use coastal seagrass and mangrove habitats as nurseries, later moving as adults onto coral reefs. But the fishes’ movements, […]

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Researchers Report Potential for a “Moderate” New England “Red Tide” in 2012

New England is expected to experience a “moderate” regional “red tide” this spring and summer, report NOAA-funded scientists working in the Gulf of Maine to study the toxic algae that causes the bloom. The algae in the water pose no direct threat to human beings, however the toxins they produce can accumulate in filter-feeding organisms such as mussels and clams— which can cause paralytic shellfish poisoning (PSP) in humans who consume them.

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