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Physical Oceanography


WHOI Scientist to Receive American Meteorological Society Award

A physical oceanographer known for his theories of wind driven ocean circulation and the fluid dynamics of the oceans will receive the 2005 Sverdrup Gold Medal from the American Meteorological Society (AMS), the nation’s leading professional society for scientists in the atmospheric and related sciences, in ceremonies January 12 at the AMS annual meeting in San Diego.

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WHOI Scientist To Receive Nansen Medal from European Geophysical Society

Kurt Polzin

Kurt Polzin, an associate scientist in the Department of Physical Oceanography at Woods Hole Oceanographic Institution, will receive the European Geophysical Society’s Fridtjof Nansen Medal in recognition of his pioneering contributions to the measurement of mixing in the deep ocean. The award will be presented at the group’s annual meeting in Nice, France, in early April.

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WHOI Scientist to be Honored January 16 by the American Meteorological Society

Nelson Hogg, a senior scientist at the Woods Hole Oceanographic Institution (WHOI), will receive the 2002 Stommel Award from the American Meteorological Society (AMS) January 16 during the society’s 82nd annual meeting in Orlando, FL. AMS is the nation’s leading professional society for scientists in the atmospheric and related sciences.

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Two WHOI Scientists Recognized with Endowed Positions

Two scientists have been recognized by the Woods Hole Oceanographic Institution (WHOI) for their contributions to ocean sciences research. Drs. Daniel J. Fornari of the Geology and Geophysics Department and Rui Xin Huang of the Physical Oceanography Department have been named recipients of a W. Van Alan Clark Chair for Excellence in Oceanography at the Institution. Each endowed chair brings financial support for a period of five years, allowing the recipient the freedom to pursue a variety of career interests. The awards were announced today during the Institution’s fall meeting of the Board of Trustees and Members of the Corporation and are effective January 1, 2002.

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Outposts in the Ocean

Oceanographers and climatologists have something in common with politicians and stock market analysts: They are all trying to get a grasp on a complex, ever-shifting system.

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Launching the Argo Armada

Launching the Argo Armada

The Argo program proposes to disperse 3,000 floats, like the one below, throughout the oceans to collect data on oceanic conditions that can be periodically transmitted to shore via satellite.

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U.S. Navy Honors Two WHOI Scientists

The Office of Naval Research (ONR) has named Senior Scientist Robert A. Weller and Associate Scientist Steven P. Anderson of the Woods Hole Oceanographic Institution (WHOI) as recipients of its…

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A New Way to Catch the Rain

The carbon budget of the upper ocean includes an important loss to the deep ocean due to a very slowly falling rain of organic particles, usually called sediment. As this sediment falls through the upper water column it is consumed, mainly by bacteria, and the carbon is recycled into nonsinking forms (dissolved or colloidal organic carbon or inorganic forms). Thus the sediment rain decreases with increasing depth in the water column, and only a tiny fraction reaches the deep sea floor, less than about one percent.

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Adventure in the Labrador Sea

Adventure in the Labrador Sea

The sound of the general alarm bell reverberated through the ship. At 2:30 AM, this couldn’t be a drill. Even more puzzling, we were still dockside in Halifax, four hours from our scheduled departure for the Labrador Sea.

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Labrador Sea Water Carries Northern Climate Signal South

Labrador Sea Water Carries Northern Climate Signal South

Changes in wind strength, humidity, and temperature over the ocean affect rates of evaporation, precipitation, and heat transfer between ocean and air. Long-term atmospheric climate change signals are imprinted onto the sea surface layer, a thin skin atop an enormous reservoirA? and subsequently communicated to the deeper water masses. Labrador Sea Water is a subpolar water mass shaped by air-sea exchanges in the North Atlantic. It is a major contributor to the deep water of the Atlantic, and changes of conditions in its formation area can be read several years later at mid-depths in the subtropics. Mapping these changes through time is helping us to understand the causes of significant warming and cooling patterns we have observed at these depths in the North Atlantic and links the subtropical deep signals back to the subpolar sea surface conditions.

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North Atlantic’s Transformation Pipeline Chills and Redistributes Subtropical Water

North Atlantic's Transformation Pipeline Chills and Redistributes Subtropical Water

Warm and salty waters from the upper part of the South Atlantic flow northward across the equator and then progress through the tropical and subtropical North Atlantic to reach high latitudes. Beginning with the intense northward flow of the Gulf Stream off the East Coast of the United States, these waters are exposed to vigorous cooling, liberating considerable oceanic heat to the atmosphere. This is the first stage of “warm water transformation within the North Atlantic, a process that culminates in the high latitude production of cold and fresh waters that return to the South Atlantic in deep reaching currents beneath the warm waters of the subtropics and tropics.

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Oceans & Climate

Oceans & Climate

The past decade has brought rapid scientific progress in understanding the role of the ocean in climate and climate change. The ocean is involved in the climate system primarily because it stores heat, water, and carbon dioxide, moves them around on the earth, and exchanges these and other elements with the atmosphere.

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The Bermuda Station S—A Long-Running Oceanographic Show

The Bermuda Station S—A Long-Running Oceanographic Show

A time series of hydrographic measurements was initiated at Bermuda in 1954 and continues to the present. It began under the banner of the International Geophysical Year (1957-1958) with the scientific support of Henry Stommel of the Woods Hole Oceanographic Institution and William Sutcliffe, director of the Bermuda Biological Station (BBS). The scientists and personnel of the originating institutions have been the most active participants over the years, but the data have been widely used by the international oceanographic community. While other long time series of measurements in the North Atlantic began in association with weather ships, only the Bermuda measurements have a strong oceanographic focus.

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