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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...
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...
Energetics of the Internal Tide on Northern Georges Bank
Internal Tide Northern Georges Bank frontal zone
2008/12/17
This paper discusses the energetics of the internal waves generated by the tide on the northern edge of Georges Bank in the outer Gulf of Maine–-a region of strong tidal flow, a density/temperature fr...
A Numerical Study of Stratified Tidal Rectification over Finite-Amplitude Banks. Part II：Georges Bank
Gulf of Maine coastal ocean circulation model Stratified Tidal Rectification Georges Bank
2008/12/12
Tidal rectification over an idealized two-dimensional cross section of Georges Bank, which is a large, shallow, elongated submarine bank in the Gulf of Maine, is studied using a primitive equation coa...