Wind-driven circulation in a shelf valley. Part I : Mechanism of the asymmetrical response to along-shelf winds in opposite directions
暂无分享,去创建一个
[1] S. S. Acquaviva,et al. The Vertical Structure , 2019, Social Structure in Italy.
[2] Glen Gawarkiewicz,et al. Dynamics of the direct intrusion of Gulf Stream ring water onto the Mid‐Atlantic Bight shelf , 2015 .
[3] Zhiqiang Liu,et al. Upwelling induced by the frictional stress curl and vertical squeezing of the vortex tube over a submerged valley in the East China Sea , 2015 .
[4] C. Harris,et al. The vertical structure of the circulation and dynamics in Hudson Shelf Valley , 2014 .
[5] B. Hickey,et al. Regional impact of submarine canyons during seasonal upwelling , 2014 .
[6] J. Kämpf. Lee effects of localized upwelling in a shelf-break canyon , 2012, CSR 2012.
[7] P. Harris,et al. Global distribution of large submarine canyons: Geomorphic differences between active and passive continental margins , 2011 .
[8] N. Walker,et al. The dynamics of the Mississippi River plume: Impact of topography, wind and offshore forcing on the fate of plume waters , 2011 .
[9] B. Hickey,et al. Dynamics of advection‐driven upwelling over a shelf break submarine canyon , 2010 .
[10] X. Durrieu de Madron,et al. A review of the role of submarine canyons in deep-ocean exchange with the shelf , 2009 .
[11] R. Chant,et al. Modeling the Pathways and Mean Dynamics of River Plume Dispersal in the New York Bight , 2009 .
[12] A. Ogston,et al. Morphology and filling of incised submarine valleys on the continental shelf near the mouth of the Fly River, Gulf of Papua , 2008 .
[13] Humfrey Melling,et al. Joint effects of wind and ice motion in forcing upwelling in Mackenzie Trough, Beaufort Sea , 2006 .
[14] J. Kämpf. Transient wind‐driven upwelling in a submarine canyon: A process‐oriented modeling study , 2006 .
[15] K. Brink. Coastal-trapped waves with finite bottom friction , 2006 .
[16] S. Smirnov,et al. The Effects of Boundary Turbulence on Canyon Flows Forced by Periodic Along-Shelf Currents , 2006 .
[17] D. Haidvogel. Cross-Shelf Exchange Driven by Oscillatory Barotropic Currents at an Idealized Coastal Canyon , 2005 .
[18] E. Baker,et al. Biological and physical processes in and around Astoria submarine Canyon, Oregon, USA , 2004 .
[19] E. Johnson,et al. ROSSBY WAVE HYDRAULICS , 2003 .
[20] C. Harris,et al. Winter-time circulation and sediment transport in the Hudson Shelf Valley , 2003 .
[21] D. Haidvogel,et al. Laboratory–Numerical Model Comparisons of Canyon Flows: A Parameter Study , 2003 .
[22] M. Breitzke,et al. Sediment transport in the shelf canyon "Swatch of No Ground" (Bay of Bengal) , 2003 .
[23] J. Klinck,et al. Flow near submarine canyons driven by constant winds , 2000 .
[24] E. Johnson,et al. Dispersive effects in Rossby-wave hydraulics , 1999, Journal of Fluid Mechanics.
[25] B. Hickey. The Response of a Steep-Sided, Narrow Canyon to Time-Variable Wind Forcing , 1997 .
[26] D. Chapman,et al. Anticyclonic eddies trapped on the continental shelf by topographic irregularities , 1997 .
[27] J. Klinck. Circulation near submarine canyons: A modeling study , 1996 .
[28] S. Fromm,et al. Observations of bottom currents and estimates of resuspended sediment transport at the New York Bight 12‐mile dumpsite , 1994 .
[29] P. Haynes,et al. A simple model of Rossby-wave hydraulic behaviour , 1993, Journal of Fluid Mechanics.
[30] K. Brink. On the damping of free coastal-trapped waves , 1990 .
[31] R. Grimshaw,et al. Frictionally Modified Continental Shelf Waves and the Subinertial Response to Wind and Deep-0cean Forcing , 1989 .
[32] J. Klinck. Geostrophic Adjustment Over Submarine Canyons , 1989 .
[33] Kenneth H. Brink,et al. Topographic Drag Due to Barotropic Flow over the Continental Shelf and Slope , 1986 .
[34] E. Baker,et al. Suspended particle movement in and around Quinault submarine Canyon , 1986 .
[35] T. Maxworthy,et al. Two-layer model of shear-driven coastal upwelling in the presence of bottom topography , 1985, Journal of Fluid Mechanics.
[36] D. Chapman. Numerical Treatment of Cross-Shelf Open Boundaries in a Barotropic Coastal Ocean Model , 1985 .
[37] J. Allen,et al. The Generation of Continental Shelf Waves by Alongshore Variations in Bottom Topography , 1979 .
[38] P. Killworth. Coastal Upwelling and Kelvin Waves with Small Longshore Topography , 1978 .
[39] D. A. Brooks,et al. Free, Stable Continental Shelf Waves in a Sheared, Barotropic Boundary Current , 1977 .
[40] C. Mooers,et al. Coastal-Trapped Waves in a Continuously Stratified Ocean , 1976 .
[41] James C. McWilliams,et al. Computational Kernel Algorithms for Fine-Scale, Multiprocess, Longtime Oceanic Simulations , 2009 .
[42] J. Kämpf. On the Interaction of Time-Variable Flows with a Shelfbreak Canyon , 2009 .
[43] D. Haidvogel. Cross-shelf Exchange Driven by Oscillatory Barotropic Currents over an Isolated Coastal Canyon : Equilibrium Circulation and Dynamics , 2003 .
[44] R. Flather. A tidal model of the north-west European continental shelf , 1976 .
[45] K. Denman. A topographically controlled upwelling center off southern Vancouver Island , 2022 .