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  • 1
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    Woods Hole Oceanographic Institution
    Publication Date: 2022-05-25
    Description: The Massachusetts Bays Program made bottom pressure and water velocity observations in Massachusetts and Cape Cod Bays during 1990 and 1991. In the Bays, the sea surface elevation appeared to rise and fall in phase with equal amplitudes at each diurnal or semidiurnal tidal frequency. There is some amplification in Boston and Provincetown harbors. The semidiurnal tides (particularly the M2 constituent) dominate. Massachusetts and Cape Cod Bays are part of the Gulf of Maine/Bay of Fundy system which is resonant near the semidiurnal frequency. This resonance amplifies the importance of the semidiurnal tides so that diurnal and higher harmonic tides become negligible. The sea level tides force currents which move with the same frequencies, but whose amplitudes are affected by the bathymetry. The strongest currents exist in the channel between Race Point and Stellwagen Bank where tidal currents exceed 1 knot. Analysis of current records for their tidal signal is complicated by internal tides which contaminate the records. These internal waves at tidal frequency exist on the stratification in the water column, and disappear during winter well-mixed times. At other times they must be considered as a signifcant source of energy for mixing and resuspension of sediments.
    Keywords: Tides ; Currents ; Internal waves
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 3845643 bytes
    Format: application/pdf
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  • 2
    Publication Date: 2022-05-25
    Description: The 1995 Geoges Bank Stratification Study (GBSS) was the first intensive process study conducted as part of the U.S. GLOBEC Northwest Atlantic/Georges Bank field program. The GBSS was designed to investigate the physical processes which control the seasonal development of stratification along the southern flank of Georges Bank during spring and summer. Past work suggested that during this period, larval cod and haddock tended to aggregate to the thermocline on the southern flank where higher concentrations of their copepod prey were found. A moored array was deployed as part of GBSS to observe the onset and evolution of sesonal stratification over the southern flank with sufficient vertical and horizontal resolution that key physical processes could be identified and quantified. Moored current, temperature, and conductivity (salinity) measurements were made at three sites along the southern flank, one on the crest, and one on the northeast peak of the bank. Moored surface meteorological measurements were also made at one southern flank site to determine the surface wind stress and heat and moisture fluxes. The oceanographic and meteorological data collected with the GBSS array during January-August 1995 are presented in this report. Meteorological data collected on National Data Buoy Center environmental buoys 44011 (Georges Bank), 44008 (Nantucket Shoals), and 44005 (Gulf of Maine) are included in this report for completeness and comparison with the GBSS southern flank meteorological measurements.
    Description: Funding was provided by the National Science Foundation under Grant Numbers OCE-98-06379 and OCE-98-06445.
    Keywords: U.S. GLOBEC ; Moored array ; Parizeau (Ship) Cruise PAR94-018 ; Parizeau (Ship) Cruise PAR95-010 ; Endeavor (Ship: 1976-) Cruise EN256 ; Endeavor (Ship: 1976-) Cruise EN259 ; Endeavor (Ship: 1976-) Cruise EN260 ; Endeavor (Ship: 1976-) Cruise EN262 ; Endeavor (Ship: 1976-) Cruise EN269 ; Endeavor (Ship: 1976-) Cruise EN271 ; Endeavor (Ship: 1976-) Cruise EN274 ; Seward Johnson (Ship) Cruise SJ95-04 ; Seward Johnson (Ship) Cruise SJ95-06 ; Seward Johnson (Ship) Cruise SJ95-08
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 4846761 bytes
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  • 3
    Publication Date: 2022-05-25
    Description: As part of the U.S. GLOBEC Northwest Atlantic/Georges Bank program, moorings were deployed on Georges Bank as part of the broad-scale survey component to help measure the temporal variability of both physical and biological characteristics on the Bank. The array consisted of a primary mooring site on the Southern Flank which was maintained for the full 5-year duration of the field program, plus secondary moorings, with fewer sensors and of shorter duration, in the well-mixed water on the Crest and in the cod/haddock spawning region on the Northeast Peak. Temperature and conductivity (salinity) were measured at 5-m intervals, ADCP velocity profiles were obtained with 1-m vertical resolution, and bio-optical packages (measuring fluorescence, optical transmission and photosynthetically active radiation) were deployed at 10-m and 40-m depths. Bottom pressure was measured at the Southern Flank site. The buoy design, sensors and mooring configuration is presented and discussed below, and the data obtained is presented and discussed in an accompanying reports “U.S. GLOBEC Georges Bank Long-Term Moored Program: Part 2 – Yearly Data Summary and Report,” and “U.S. GLOBEC Georges Bank Long-Term Moored Program: Part 3 – Data Summary.”
    Description: Funding was provided by the National Science Foundation under grant numbers OCE-93-13670, OCE-96-32348, OCE98-06379, OCE-98-06445 and OCE-02-27679.
    Keywords: GLOBEC ; Moorings ; Georges Bank ; Oceanus (Ship : 1975-) Cruise OC256 ; Oceanus (Ship : 1975-) Cruise OC276 ; Oceanus (Ship : 1975-) Cruise OC291 ; Oceanus (Ship : 1975-) Cruise OC321 ; Oceanus (Ship : 1975-) Cruise OC331 ; Oceanus (Ship : 1975-) Cruise OC333 ; Oceanus (Ship : 1975-) Cruise OC338 ; Seward Johnson (Ship) Cruise SJ95-04 ; Seward Johnson (Ship) Cruise SJ95-06 ; Knorr (Ship : 1970-) Cruise KN149 ; Endeavor (Ship: 1976-) Cruise EN208
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 2703311 bytes
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  • 4
    Publication Date: 2022-05-26
    Description: Author Posting. © IEEE, 2004. This article is posted here by permission of IEEE for personal use, not for redistribution. The definitive version was published in IEEE Journal of Oceanic Engineering 29 (2004): 1075-1086, doi:10.1109/JOE.2004.833226.
    Description: A moored array deployed across the shelf break in the northeast South China Sea during April-May 2001 collected sufficient current and pressure data to allow estimation of the barotropic tidal currents and energy fluxes at five sites ranging in depth from 350 to 71 m. The tidal currents in this area were mixed, with the diurnal O1 and K1 currents dominant over the upper slope and the semidiurnal M2 current dominant over the shelf. The semidiurnal S2 current also increased onshelf (northward), but was always weaker than O1 and K1. The tidal currents were elliptical at all sites, with clockwise turning with time. The O1 and K1 transports decreased monotonically northward by a factor of 2 onto the shelf, with energy fluxes directed roughly westward over the slope and eastward over the shelf. The M2 and S2 current ellipses turned clockwise and increased in amplitude northward onto the shelf. The M2 and S2 transport ellipses also exhibited clockwise veering but little change in amplitude, suggesting roughly nondivergent flow in the direction of major axis orientation. The M2 energy flux was generally aligned with the transport major axis with little phase lag between high water and maximum transport. These barotropic energy fluxes are compared with the locally generated diurnal internal tide and high-frequency internal solitary-type waves generated by the M2 flow through the Luzon Strait.
    Description: This work was supported by the U.S. Office of Naval Research under Grant N00014-98-1-0210 to the Woods Hole Oceanographic Institution and under Grant N00014-01-WR20044 to the Naval Postgraduate School.
    Keywords: Sea measurements ; South China Sea ; Tidal currents ; Tides
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: 1316461 bytes
    Format: application/pdf
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