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New Study Definitively Confirms Gulf Stream Weakening

Lisa Beal communicating to the bridge

The Gulf Stream – which is a major ocean current off the U.S. East Coast and a part of the North Atlantic Ocean circulation – plays an important role in weather and climate, and a weakening could have significant implications.

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How marine predators find food hot spots in open ocean “deserts”

A new study led by scientists at Woods Hole Oceanographic Institution (WHOI) and University of Washington Applied Physics Laboratory (UW APL) finds that marine predators, such as tunas, billfishes and sharks, aggregate in anticyclonic, clockwise-rotating ocean eddies (mobile, coherent bodies of water). As these anticyclonic eddies move throughout the open ocean, the study suggests that the predators are also moving with them, foraging on the high deep-ocean biomass contained within.

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WHOI & Pangaea Logistics Solutions to advance ocean science data acquisition through Science RoCS program

WHOI and Pangaea Logistics Solutions (Pangaea), a U.S. based, international maritime and logistics transportation company, today announced the launch of a new science program aboard Pangaea’s fleet of ships. Science RoCS (Science Research on Commercial Ships) is an innovative program pairing scientists with commercial vessels to regularly monitor the vast and open ocean, particularly along repeat routes in hard-to-reach areas where critical gaps in monitoring exist.

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Tropical fish…up north? How ocean physics play a role in altering water temperature and salinity

A study led by Woods Hole Oceanographic Institution scientists is explaining why warm and salty water along with warm water fish species, such as the deep-sea dwelling Gulf Stream flounder and Black Sea bass, were found far inshore in New England in the middle of winter 2017. How did this happen? Researchers say it is due to an intrusion of offshore water from the open ocean onto the Northeast U.S. Shelf, caused by eddies (a circular current of water) and wind.

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Modeling our climate future; WHOI to lead ocean current research

Woods Hole Oceanographic Institution (WHOI) senior scientist of physical oceanography, Dr. Young-Oh Kwon, and WHOI adjunct scientist, Dr. Claude Frankignoul, have received a new research grant from the National Oceanic and Atmospheric Administration (NOAA) Modeling, Analysis, Predictions and Projections (MAPP) Program, funding their research project focusing on western boundary ocean currents and their correspondence with the atmosphere in relation to modern day climate.

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A rapidly changing Arctic

Healy, Polarstern

A new study by researchers at Woods Hole Oceanographic Institution (WHOI) and their international colleagues found that freshwater runoff from rivers and continental shelf sediments are bringing significant quantities of carbon and trace elements into parts of the Arctic Ocean via the Transpolar Drift—a major surface current that moves water from Siberia across the North Pole to the North Atlantic Ocean.

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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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Waters West of Europe Drive Ocean Overturning, Key for Regulating Climate

Waters West of Europe Drive Ocean Overturning, Key for Regulating Climate

In the Atlantic MOC, warm, salty, shallow waters are carried northward from the tropics by currents and wind, and then converted into colder, fresher, deep waters that return southward through the Iceland and Irminger basins. In a departure from the prevailing scientific view, the study shows that most of the conversion from warm to cold water – or ‘overturning’™ and its month-to-month variability – ”is occurring in regions between Greenland and Scotland, rather than in the Labrador Sea off Canada, as many past modeling studies have suggested.

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