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The steady-state circulation in a rectangular bay is studied numerically in a model of homogeneous water and vertical coasts. The competing influences of the surface winds and longshore currants flowi...
The Noutidal Flow in the Providence River of Narragansett Bay：A Stochastic Approach to Estuarine Circulation
Noutidal Flow Narragansett Bay Providence River Estuarine Circulation
2009/3/7
Atmospherically driven flow in the Providence River (a partially mixed estuary) has been examined using a 51-day velocity record measured 2 m from the bottom. Velocity fluctuations at time scales betw...
Velocity Observations in the West Passage of Narragansett Bay：A Partially Mixed Estuary
West Passage of Narragansett Bay A Partially Mixed Estuary
2009/3/7
Narragansett Bay is a weakly stratified estuary comprised of three connecting passages of varying depths. The vertical distribution of horizontal velocity was observed in the West Passage using moored...
Non-Tidal Variability in the Chesapeake Bay and Potomac River：Evidence for Non-Local Forcing
Non-Tidal Variability Chesapeake Bay Potomac River Non-Local Forcing
2009/2/23
Non-tidal variability in the Chesapeake Bay and Potomac River, and its relation to atmospheric forcing, is examined from two-month sea level and bottom current measurements. The dominant sea level flu...
Wind-Driven Circulation in the Chesapeake Bay, Winter, 1975
Wind-Driven Circulation Chesapeake Bay
2009/2/13
Nontidal circulation in Chesapeake Bay was examined from one-month current records at 50 and 200 km from the entrance. The monthly mean flow was basically a two-layered circulation; in addition, there...
Subtidal Sea Level Variations in the Chesapeake Bay and Relations to Atmospheric Forcing
Subtidal Sea Level Atmospheric Forcing Chesapeake Bay
2009/2/13
Subtidal sea level variations in the Chesapeake Bay were examined over a one-year period for evidence of wind-driven barotropic circulation. The major transport occurred at time scales of 3–5 days, wh...
On Lateral Water Mass Interaction—A Case Study, Bristol Bay, Alaska
Lateral Water Mass Interaction Bristol Bay Alaska
2009/2/13
Salinity-temperature-depth data obtained on several spring and summer cruises during 1976 and 1977 from outer Bristol Bay in the southeast Bering Sea indicate the existence of a zone, between two well...
Gulf Stream Fluctuations and Meanders over the Onslow Bay Upper Continental Slope
sea surface temperature Onslow Bay Upper Continental Slope
2009/2/9
Gulf Stream fluctuations observed over the 200 and 400 m isobaths off Onslow Bay, North Carolina have a prominent weekly time scale. The principal fluctuations observed during the 4-month winter exper...
Low-Frequency Variations in Sea Level and Currents in South San Francisco Bay
Low-Frequency South San Francisco Bay Sea Level
2009/2/7
In order to examine physical process in the subtidal time range, sea-level and current meter data for south San Francisco Bay (South Bay) were filtered using a low-pass digital filter to remove tidal ...
Laboratory Models of Bay-Type Continental Shelves in the Winter
Bay-Type Continental Shelves shallow sea depth bounded
2009/2/6
A laboratory experiment consisting of a shallow sea of constant depth bounded by a deep ocean through a uniformly sloping continental rise was conducted. The experiment is cooled from above, and there...
Modelling the Mean Barotropic Circulation in the Bay of Fundy and Gulf of Maine
nonlinear numerical models multi-grid model
2009/2/5
Two dimensional, nonlinear numerical models are used to study the residual barotropic circulation generated by tides and steady winds in the Bay of Fundy and Gulf of Maine. The first a multi-grid mode...
Observations of Low-Frequency Variability in Great South Bay and Relations to Atmospheric Forcing
Low-Frequency Variability Great South Bay Atmospheric Forcing
2009/1/21
Sea level and current data collected around Great South Bay, New York during December 1979 are examined in conjunction with atmospheric data for evidence of wind-forced, low frequency variability in t...
Wind-Induced Destratification in Chesapeake Bay
Wind-Induced Destratification Chesapeake Bay
2009/1/9
Multiyear continuous observations of velocity and salinity in the Chesapeake Bay indicate that wind-induced destratification occurs frequently from early fall through midspring over large areas of the...
Abyssal Penetration and Bottom Reflection of Internal Tidal Energy in the Bay of Biscay
Internal Tidal Energy Bottom Reflection
2008/12/23
This paper describes field observations in the Bay of Biscay, and presents convincing evidence for the existence of a broad beam of internal tidal energy propagating downward from a source region on t...
A Latent-and Sensible-Heat Polynya Model for the North Water, Northern Baffin Bay
North Water A Latent-and Sensible-Heat Polynya Northern Baffin Bay
2008/12/22
The Pease latent-heat polynya model is coupled to a reduced-gravity, coastal upwelling model in order to simulate the formation and maintenance of the North Water (NOW), the Arctic's largest polynya, ...