The effect of wind-wave enhancement of bottom stress on the circulation induced by tropical cyclones on continental shelves

Journal of Geophysical Research: Oceans

Volumn 101, Issue C10, 1996, Pages 22705-22714

  Tang, Yong Ming ^a,c   Grimshaw, Roger ^b  

^a BUREAU OF METEOROLOGY RESEARCH CENTRE   (Australia)

^b MONASH UNIVERSITY   (Australia)

^c BUREAU OF METEOROLOGY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

BOTTOM STRESS; SHELF DYNAMICS; TROPICAL CYCLONES; WIND WAVES;

EID: 0030424168     PISSN: 01480227     EISSN: None     Source Type: Journal    
DOI: 10.1029/96JC02002     Document Type: Article

References (6)

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3. Clarke, A. J., and K. H. Brink, The response of stratified frictional flow of shelf and slope waters to fluctuating large-scale, low frequency wind forcing, J. Phys. Oceanogr., 15, 439-453, 1985.
4. Cooper, C., and J. D. Thompson, Hurricane-generated currents on the outer continental shelf, 1, Model formulation and verification, J. Geophys. Res., 94, 12,513-12,539, 1989.
5. Davies, A. M., and J. Lawrence, Examining the influence of wind and wind wave turbulence on tidal currents, using a three-dimensional hydrodynamic model including wave-current interaction, J. Phys. Oceanogr., 24, 2441-2460, 1994.
6. Davies, A. M., and J. Lawrence, Modeling the effect of wavecurrent interaction on the three-dimensional wind-driven circulation of the eastern Irish Sea, J. Phys. Oceanogr., 25, 29-45, 1995.