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Observations of tidal variablity on the New England shelf

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Title Observations of tidal variablity on the New England shelf
Names Shearman, R. Kipp (creator)
Lentz, Steven J. (creator)
Date Issued 2004-06-04 (iso8601)
Note Copyrighted by American Geophysical Union.
Abstract Observations from the Coastal Mixing and Optics experiment moored array, deployed
from August 1996 through June 1997, are used to describe barotropic and baroclinic
tidal variability over the New England shelf. The dominant M₂ tidal elevations decrease
toward the northeast to a minimum over the Nantucket shoals (about 34 cm), and
barotropic tidal current amplitudes increase strongly toward the northeast to a maximum
over the shoals (about 35 cm s⁻¹). Estimates of the depth-averaged M₂ momentum balance
indicate that tidal dynamics are linear, and along-shelf pressure gradients are as large
as cross-shelf pressure gradients. In addition, tidal current ellipses are weakly polarized,
confirming that the dynamics are more complex than simple plane waves. The vertical
structure of the M₂ currents decreases in amplitude and phase (phase lead near bottom)
over the bottom 20 m. The M₂ momentum deficit near the bottom approximately
matches direct covariance estimates of stress, confirming the effects of stress on current
structure in the tidally driven bottom boundary layer. Baroclinic current variability at
tidal frequencies is small (2 cm s⁻¹ amplitude), with a predominantly mode 1 vertical
structure. High-frequency (approaching the buoyancy frequency) internal solitons are
observed following the pycnocline. The internal solitons switch from waves of depression
to waves of elevation when the depth of maximum stratification is deeper than half the
water column depth. Both low-mode baroclinic tidal and high-frequency internal wave
energy decrease linearly with bottom depth across the shelf.
Genre Article
Topic continental shelf
Identifier Shearman, R. K., and S. J. Lentz (2004), Observations of tidal variability on the New England shelf, J. Geophys. Res., 109, C06010.

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