Effects of mass source/sink at the western boundary on the wind-driven gyres: Implications for the ventilation of the north pacific intermediate layer through convection in the Okhotsk Sea and tidal mixing at the Kuril Straits
Author:
Publisher
Springer Science and Business Media LLC
Subject
Oceanography
Link
http://link.springer.com/content/pdf/10.1007/s10872-010-0004-1.pdf
Reference60 articles.
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2. Aoki, K. and K. Kutsuwada (2008): Verification of the winddriven transport in the North Pacific subtropical gyre using gridded wind-stress products. J. Oceanogr., 64, 49–60.
3. Aramaki, T., S. Watanabe, T. Kuji and M. Wakatsuchi (2001): The Okhotsk-Pacific seawater exchange in the viewpoint of vertical profiles of radiocarbon around the Bussol’ Strait. Geophys. Res. Lett., 28, 3971–3974.
4. Bower, A. S. and H. D. Hunt (2000): Lagrangian observations of the deep western boundary current in the North Atlantic Ocean. Part I: Large-scale pathways and spreading rates. J. Phys. Oceanogr., 30, 764–783.
5. Cember, R. P. (1998): On deep western boundary currents. J. Geophys. Res., 103, 5397–5417.
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