4.3 Article

High-resolution surface salinity maps in coastal oceans based on geostationary ocean color images: quantitative analysis of river plume dynamics

Journal

JOURNAL OF OCEANOGRAPHY
Volume 74, Issue 3, Pages 287-304

Publisher

SPRINGER
DOI: 10.1007/s10872-017-0459-4

Keywords

Sea surface salinity; Coastal oceans; Chromophoric dissolved organic matter; River plume; Typhoon; Geostationary ocean color satellite; Osaka Bay

Categories

Funding

  1. Fund of the Japan Society for the Promotion of Science [26887025, 16K13882]
  2. Kurita Water and Environment Foundation (KWEF), Japan
  3. Grants-in-Aid for Scientific Research [17K15302, 26887025, 16K13882] Funding Source: KAKEN

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Sea surface salinity (SSS) in coastal oceans is a direct indicator of riverine plumes and provides essential information about the ocean environment and ecosystem, which affects coastal fisheries, aquaculture, and marine harvests. However, to accurately capture SSS patterns in coastal oceans, high temporal and spatial resolutions are required. This paper introduces a methodology to produce high-resolution ( 500 m) SSS maps for analysis of river plumes in coastal oceans based on hourly chromophoric dissolved organic matter data collected by the Geostationary Ocean Color Imager. Osaka Bay, located in the eastern Seto Inland Sea, was selected as a pilot region. A comparison between the initial estimates and calibrated SSS data showed a substantial decrease in estimation error, by up to 71%, over a wide range of salinity (20-34) using in situ SSS data collected through an automated observation system. Calculating the salinity anomaly based on the SSS map to identify plume areas, we evaluated the impact of a large runoff event induced by a super typhoon on the river plumes. After the plume formed in the estuary, it extended southward to the bay mouth along the southeastern coast. The plume area during the post-typhoon period covered half of the bay, approximately 1.5 times the area during the pre-typhoon period. The post-typhoon, low-SSS period continued for approximately 2 weeks. Our approach can be of practical use for analyzing the dynamics of river plumes in coastal oceans, leading to the development of coastal ocean prediction models related to operational oceanography.

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