Baroclinic and barotropic tides in the Ross Sea

Publication Status is "Submitted" Or "In Press: 
Yes
LDEO Publication: 
Yes
Publication Type: 
Year of Publication: 
2005
Authors: 
Editor: 
Journal Title: 
Antarctic Science
Journal Date: 
Mar
Place Published: 
Tertiary Title: 
Volume: 
17
Issue: 
1
Pages: 
107-120
Section / Start page: 
Publisher: 
ISBN Number: 
0954-1020
ISSN Number: 
Edition: 
Short Title: 
Accession Number: 
ISI:000228018700015
LDEO Publication Number: 
6593
Call Number: 
Abstract: 

The barotropic and baroclinic tides in the Ross Sea were simulated using a primitive equation, sigma-coordinate model, the Regional Ocean Model System (ROMS), for four tidal constituents, M-2, S-2, K-1, and O-1. Small elevation amplitudes were predicted over most of the basin, with a combined standard deviation of 30-50 cm. Larger amplitudes, with standard deviations ranging from 50-70 cm, occurred deep within the ice shelf cavity, over the continental slope, and over Iselin Bank. Most of the elevation response was associated with the diurnal constituents (K-1 and O-1), as was most of the depth-independent (barotropic) velocity response. Baroclinic tides were generated at locations of steep topography for the semidiurnal constituents, but not the diurnal. Diurnal continental shelf waves were generated by the diurnal tides and found to amplify the semidiurnal elevations and baroclinic tidal velocities over the continental slope. Comparisons with observations in both elevation and velocities showed very good agreement for the semidiurnal constituents (M-2 and S-2) and moderate agreement for the diurnal constituents (K-1 and O-1). The disagreement for the diurnal constituents was associated with diurnal frequency continental shelf waves, which were overexcited along the shelf break. The baroclinic tides induced both small-scale horizontal and vertical shear in the velocity fields in the Ross Sea.

Notes: 

911QFTimes Cited:5Cited References Count:33

DOI: 
Doi 10.1017/S0954102005002506