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Observations of near-inertial curent variability on the New England shelf

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Title Observations of near-inertial curent variability on the New England shelf
Names Shearman, R. Kipp (creator)
Date Issued 2005-02-17 (iso8601)
Note Copyrighted by American Geophysical Union.
Abstract Observations from the Coastal Mixing and Optics (CMO) moored array (deployed
from August 1996 through June 1997) and supplemental moored observations are used to
describe near-inertial current variability over the New England shelf. Near-inertial band
current variance comprises 10–20% of the total observed current variance, and has
episodic peak speeds exceeding 30 cm s⁻¹. Near-inertial current variability during CMO is
characterized by a first baroclinic mode vertical structure with one zero-crossing between
15 and 50 m. The zero-crossing is shallower during periods of stronger stratification.
Laterally, near-inertial variability is coherent over the extent of the CMO moored array,
and cross-shelf decorrelation scales for near-inertial currents are about 100 km,
approximately the entire shelf width. The magnitude of near-surface near-inertial
variability is stronger in the summer and weaker in the winter, following the seasonal
variation in stratification and opposite the seasonal cycle in wind stress variance. During
CMO, near-surface near-inertial kinetic energy is inversely related to surface mixed layer
depth. Near-inertial variance decreases onshore, matching approximately the cross-shelf
decrease in near-inertial energy predicted by a two-dimensional, linear, flat-bottom, two-layer,
coastal wall model. In this model, the nullifying effects of a baroclinic wave
emanating from the coastal wall play a dominant role in controlling the onshore decrease.
Finally, strong persistent anticyclonic relative vorticity shifts near-inertial variability on
the New England shelf to subinertial frequencies.
Genre Article
Topic internal waves
Identifier Shearman, R. K. (2005), Observations of near-inertial current variability on the New England shelf, J. Geophys. Res., 110, C02012. doi:10.1029/2004JC002341

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