Three-dimensional structure of temperature, salinity, and Velocity of the summertime Vietnamese upwelling system in the South China Sea on the interannual timescale

• Vertical hydrographic profiles between mean and strong upwelling conditions in Vietnamese upwelling system are analyzed. • Contribution of dynamic effects to the upwelling process is quantified based on omega equation. • Kinematic deformation is the main contributor to coastal upwelling, while momentum plays the major role for offshore upwelling. • Southern coastal upwelling is sensitive to momentum, while northern one is controlled by kinematic deformation and momentum. Summertime upwelling system off the southern Vietnamese coast is one of the most essential oceanographic features in the South China Sea. This system is divided into two regions along the coast, the Southern Coastal Upwelling (SCU; south of 12.5°N) and Northern Coastal Upwelling (NCU; north of 12.5°N), and one in the offshore area, the Offshore Upwelling (OU; east of 110°E). Utilizing the HYCOM ocean reanalysis product in the period of 1994–2015, vertical characteristics of this upwelling system on the interannual timescale are investigated. Furthermore, the omega equation is applied to reconstruct vertical velocity to quantify its intensity and clarify the corresponding leading factors in the three regions. The analysis indicates that the kinematic deformation effect is the primary contributor to coastal upwelling formation while the momentum effect plays the leading role in offshore upwelling. The SCU variability is more sensitive to the momentum effect; however, in the NCU, the kinematic deformation effect is offset by the momentum effect and the upwelling is enhanced as the kinematic deformation (momentum) effect increases (decreases). The summertime mean vertical velocities in the central areas of SCU, NCU, and OU are estimated at 0.16 m/d, −0.08 m/d, and 0.003 m/d, respectively. The vertical velocity speeds up to 0.32 m/d, 0.07 m/d, and 0.08 m/d as the strong upwelling event occurs.

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Publication Details

Journal
Progress In Oceanography
Published
2024-09-23
DOI
https://doi.org/10.1016/j.pocean.2024.103354
Citations
3
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
Field-Weighted Citation Impact
1.44
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article

Three-dimensional structure of temperature, salinity, and Velocity of the summertime Vietnamese upwelling system in the South China Sea on the interannual timescale

Yi‐Chia Hsin, Mai‐Han Ngo
3 citations
Progress In Oceanography
Oceanographic and Atmospheric Processes
1.44
article

Three-dimensional structure of temperature, salinity, and Velocity of the summertime Vietnamese upwelling system in the South China Sea on the interannual timescale

Yi‐Chia Hsin, Mai‐Han Ngo
article en
3 citations

Abstract

• Vertical hydrographic profiles between mean and strong upwelling conditions in Vietnamese upwelling system are analyzed. • Contribution of dynamic effects to the upwelling process is quantified based on omega equation. • Kinematic deformation is the main contributor to coastal upwelling, while momentum plays the major role for offshore upwelling. • Southern coastal upwelling is sensitive to momentum, while northern one is controlled by kinematic deformation and momentum. Summertime upwelling system off the southern Vietnamese coast is one of the most essential oceanographic features in the South China Sea. This system is divided into two regions along the coast, the Southern Coastal Upwelling (SCU; south of 12.5°N) and Northern Coastal Upwelling (NCU; north of 12.5°N), and one in the offshore area, the Offshore Upwelling (OU; east of 110°E). Utilizing the HYCOM ocean reanalysis product in the period of 1994–2015, vertical characteristics of this upwelling system on the interannual timescale are investigated. Furthermore, the omega equation is applied to reconstruct vertical velocity to quantify its intensity and clarify the corresponding leading factors in the three regions. The analysis indicates that the kinematic deformation effect is the primary contributor to coastal upwelling formation while the momentum effect plays the leading role in offshore upwelling. The SCU variability is more sensitive to the momentum effect; however, in the NCU, the kinematic deformation effect is offset by the momentum effect and the upwelling is enhanced as the kinematic deformation (momentum) effect increases (decreases). The summertime mean vertical velocities in the central areas of SCU, NCU, and OU are estimated at 0.16 m/d, −0.08 m/d, and 0.003 m/d, respectively. The vertical velocity speeds up to 0.32 m/d, 0.07 m/d, and 0.08 m/d as the strong upwelling event occurs.

Progress In OceanographyVol. 229
National Central University (TW), Institute of Information Science, Academia Sinica (TW), Research Center for Applied Science, Academia Sinica (TW), Research Center for Environmental Changes, Academia Sinica (TW), Research Center for Humanities and Social Sciences, Academia Sinica (TW)
Life below water
Openalex Percentile: Top 19%
Oceanographic and Atmospheric Processes
1.44
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