Subtidal circulation on the Scotian Shelf: Assessing the hindcast skill of a linear, barotropic model

Journal of Geophysical Research: Oceans

Volumn 102, Issue C11, 1997, Pages 24987-25003

  Thompson, Keith R ^a   Sheng, Jinyu ^a  

^a DALHOUSIE UNIVERSITY   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

BAROTROPIC MODEL; CONTINENTAL SHELF; SEA LEVEL; WATER CIRCULATION; WIND STRESS;

ATLANTIC, SCOTIAN SHELF;

EID: 0031403047     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/97JC00368     Document Type: Article

References (6)

1. Akaike, H., A new look at the statistical model identification, IEEE Trans. Autom. Control, AC-19, 6, 716-723, 1974.
2. Anderson, C., and P. C. Smith, Oceanographic observations on the Scotian Shelf during CASP, Atmos. Ocean, 27, 130-156, 1989.
3. Chapman, D. C., Numerical treatment of cross-shelf open boundaries in a barotropic coastal ocean model, J. Phys. Oceanogr., 15, 1060-1075, 1985.
4. Csanady, G. T., The arrested topographic wave, J. Phys. Oceanogr., 8, 47-62, 1978.
5. Csanady, G. T., The pressure field along the western margin of the North Atlantic, J. Geophys. Res., 84, 4905-4915, 1979.
6. De Young, B., Youyu Lu, and R. Greatbatch, Synoptic bottom pressure variability on the Labrador and Newfoundland continental shelves, J Geophys. Res., 100, 8639-8653, 1995.