Thermohaline finestructure observed near the northern Philippine coast

Fan Wang; Yuanlong Li

doi:10.1007/s00343-012-1246-0

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Thermohaline finestructure observed near the northern Philippine coast

Updated：2023-05-16

- Thermohaline finestructure observed near the northern Philippine coast
- Journal of Oceanology and Limnology Vol. 30, Issue 6, Pages: 1033-1044(2012)
- Affiliations：
  
  1. Key Laboratory of Ocean Circulation and Waves Institute of Oceanology Chinese Academy of Sciences
  2. Graduate University of Chinese Academy of Sciences
- Author bio：
- Funds：
- DOI：10.1007/s00343-012-1246-0
  CLC：
- Online First：17 November 2012，
  
  Published：2012
- Accepted：
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Wang, F., Li, Y. Thermohaline finestructure observed near the northern Philippine coast., Chin. J. Ocean. Limnol. 30, 1033–1044 (2012). https://doi.org/10.1007/s00343-012-1246-0
DOI：

Wang, F., Li, Y. Thermohaline finestructure observed near the northern Philippine coast., Chin. J. Ocean. Limnol. 30, 1033–1044 (2012). https://doi.org/10.1007/s00343-012-1246-0 DOI：

摘要

Abstract

Using hydrographic measurements from three recent surveys in the western tropical Pacific

this study revealed the existence and general features of thermohaline finestructure near the northern Philippine coast. Pronounced finestructures were detected in the layers of the North Pacific Tropical Water (NPTW) and the North Pacific Intermediate Water (NPIW) during all three cruises and shown to be mainly thermohaline intrusions. Characteristics of the intrusions were further investigated with spiciness curvature and salinity anomaly methods. The vertical scale of the intrusions was 20–50 m and 50–100 m in the NPTW and NPIW layers

respectively. Within the NPTW layer

the Turner angle distribution and correlation between salinity and density anomalies suggested that diffusive convection between surface fresh water and subsurface saline water played an important role in the development and maintenance of the intrusions. In addition

connection between thermohaline finestructure and larger-scale oceanic processes was explored using historical hydrographic data. The results reveal that the salinity field and the distribution of the intrusions in this region were largely determined by mesoscale eddies. As a result of eddy stirring

both isopycnal and diapycnal temperature/salinity gradients were strengthened

which gave rise to the development of thermohaline intrusions. The intrusions acted to enhance heat and salt fluxes and resulted in the mixing of water masses being more efficient. By linking mesoscale eddy stirring to micro-scale diffusion

thermohaline finestructure plays a vital role in the ocean energy cascade and water mass conversion in the northern Philippine Sea.

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