Observations on the evolution of tidal vorticity at a stratified deep water headland-Reference-Cited by-同舟云学术

Observations on the evolution of tidal vorticity at a stratified deep water headland

Published:2003-12 Issue:24 Volume:30 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Pawlak G.¹,MacCready P.²,Edwards K. A.³,McCabe R.²

Affiliation:

1. Department of Ocean and Resources Engineering; University of Hawaii at Manoa; Honolulu Hawaii USA

2. School of Oceanography; University of Washington; Seattle Washington USA

3. Applied Physics Laboratory; University of Washington; Seattle Washington USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference14 articles.

1. Form drag and mixing due to tidal flow past a sharp point;Edwards;J. Phys. Oceanogr.,2003

2. Lavelle , J. W. A multiply-connected channel model of tides and tidal currents in Puget Sound, Washington and a comparison with updated observations Tech. Rep. NOAA Tech. Memo. ERL PMEL-84 1988

3. Stratified flow along a corrugated slope: Separation drag and wave drag;MacCready;J. Phys. Oceanogr.,2001

4. Determination of vorticity, divergence, and deformation rates from analysis of drogue observations;Okubo;Deep Sea Res.,1976

5. Oscillatory flow across an irregular boundary;Pawlak;J. Geophys Res.,2001

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