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Working to Protect Biodiversity:Stellwagen Bank National Marine Sanctuary
Protect Biodiversity Stellwagen Bank National Marine Sanctuary
2015/8/13
At the Stellwagen Bank National Marine Sanctuary, protecting marine biodiversity while supporting sustainable uses is a multipronged effort involving research, education, and enforcement. Located on t...
The Straits of Florida is a trough that separates the Florida
Peninsula from Cuba and the Great Bahama Bank (Figure 1).
It acts as both a conduit and a barrier for ecosystem exchange
and is an i...
Ecology of a Chaetoceros socialis Lauder Patch on Georges Bank: Distribution, Microbial Associations, and Grazing Losses
Georges Bank: Distribution Microbial Associations
2015/8/6
The presence of patches and layers in marine pelagic ecosystems may play an important role in providing food for higher trophic levels at concentrations high enough to support the metabolism, growth, ...
Real-Time Data Assimilative Modeling on Georges Bank
Real-Time Data Assimilative Georges Bank
2015/8/4
Real-time oceanic forecasts were constructed at sea on Georges Bank during Spring 1999. Ship- and shorebased computations were combined to deliver daily 3-day forecasts to shipboard scientists for int...
The cold-water coral community as a hot spot for carbon cycling on continental margins: A food-web analysis from Rockall Bank (northeast Atlantic)
The cold-water coral community carbon cycling continental margins: A food-web analysis Rockall Bank
2014/4/17
We present a quantitative food-web analysis of the cold-water coral community, i.e., the assembly of living corals, dead coral branches and sediment beneath, associated with the reef-buildingLophelia ...
Topographic Rectification of Tidal Currents on the Sides of Georges Bank
Topographic Rectification Georges Bank Tidal Currents
2009/2/18
The rectification of M2 tidal currents on the sloping sides of Georges Bank is predicted to make an important year-round contribution to its observed mean clockwise circulation. A rectification mechan...
The Relationship of Tidal and Low-Frequency Currents on the North Slope of Georges Bank
Tidal Low-Frequency Currents North Slope of Georges Bank
2009/2/18
Measured currents at the steeply sloping north edge of Georges Bank show an unusually strong correlation between tidal and lower frequency components. The dominant current constituents are the rotary ...
An Upper Bound for the Tidally Rectified Current at One Location on the Southern Flank of Georges Bank
Upper Bound Georges Bank Tidally Rectified Current
2009/2/6
Long-term current observations at 45 and 75 m at one location on the southern flank of Georges Bank in water 85 m deep were examined for evidence of tidal rectification. Loder has shown analytically t...
Low-Frequency Free Wave and Wind-Driven Motions Over a Submarine Bank
Low-Frequency Free Wave Wind-Driven Motions Submarine Bank
2009/1/21
This study attempts to isolate the physics peculiar to a submarine bank. The particular model is barotropic and contains an infinitely long straight bank within an unbounded ocean basin. The low-frequ...
A Comparison of Georges Bank, Gulf of Maine and New England Shelf Tidal Dynamics
Georges Bank semidiurnal tidal currents Shelf Tidal Dynamics
2009/1/19
The semidiurnal tidal currents associated with the near-resonant response of the Gulf of Maine-Bay of Fundy system are amplified over the relatively shallow depths of Georges Bank, thus leading to enh...
Depth-Dependent Studies of Tidally Induced Residual Currents on the Sides of Georges Bank
Tidally Induced Residual Currents Georges Bank
2009/1/16
Using a depth-dependent tidal model, the tidally induced residual currents on the northern and southern sections of Georges Bank are computed and the effects of various physical parameters on the curr...
Wind–Current Coupling on the Southern Flank of Georges Bank：Variation with Season and Frequency
Wind–Current Coupling Georges Bank Southern Flank
2009/1/15
Comparison of several years of current observations on the southern flank of Georges Bank with nearby wind data shows that the wind–current coupling is primarily between longshelf wind stress and long...
Long-Term Observations on the Southern Flank of Georges Bank. Part I：A Description of the Seasonal Cycle of Currents, Temperature, Stratification, and Wind Stress
Long-Term Observations Georges Bank Seasonal Cycle Wind Stress
2009/1/7
Nearly continuous current measurements at 45 and 75 m were made from May 1975 to March 1979 at 40°51′N, 67°24′W on the southern flank of Georges Bank in water 85 m deep. Measurements at 15 and 84 m we...
Storm-Forced Baroclinic Near-Inertial Currents on the Grand Bank
Grand Bank inertial currents Storm-Forced Baroclinic
2008/12/30
Current meter data for six mouths from the Grand Bank are analyzed to study inertial currents generated by moving storms. It is found that during periods of strong winds, but no well-defined storm sys...
Cold Outflow from the Faroe Bank Channel
Acoustic Doppler Current Profiler Cold Outflow Faroe Bank Channel
2008/12/27
The exchange of water between the Norwegian Sea and the North Atlantic around the Faroe Islands was investigated in 1987 and 1988 combining CTD data with shipborne Acoustic Doppler Current Profiler (A...