Wind Relaxation as a Possible Cause of the South China Sea Warm Current
スポンサーリンク
概要
著者
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Chao S‐y
Univ. Maryland Center For Environmental Sci. Maryland Usa
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Chao Shenn-yu
Horn Point Environmental Laboratory University Of Maryland
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Shaw P‐t
North Carolina State Univ. North Carolina Usa
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Shaw Ping-tung
Department Of Marine Earth And Atmospheric Sciences North Carolina State University
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WANG JOE
Institute of Oceanography, National Taiwan University
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Wang Joe
Institute Of Oceanography National Taiwan University
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Chao Shenn-Yu
Horn Point Environmental Laboratories, University of Maryland
関連論文
- Reflection and Diffraction of Internal Solitary Waves by a Circular Island
- Assessing the West Ridge of Luzon Strait as an Internal Wave Mediator
- Fission of Heton-like Vortices under Sea Ice
- Circulation and Brackish Water Dispersal in a Coastal Lagoon of Southwest Taiwan
- Transition of Tidal Waves from the East to South China Seas over the Taiwan Strait : Influence of the Abrupt Step in the Topography
- Tidally Induced Upwelling in a Semi-Enclosed Basin: Nan Wan Bay
- Cold Deep Water in the South China Sea
- Numerical Study of the Upper-Layer Circulation in the South China Sea
- Seasonal and Interannual Variations in the Velocity Field of the South China Sea
- Transient, Seasonal and Interannual Variability of the Taiwan Strait Current
- Interactions of Mesoscale Eddy and Western Boundary Current : A Reduced-Gravity Numerical Model Study
- Wind Relaxation as a Possible Cause of the South China Sea Warm Current
- Some aspects on the circulation in the northern South China Sea
- The Upper Ocean Response to a Moving Typhoon
- A Numerical Study of the Summertime Flow around the Luzon Strait