Time series changes in sea-surface temperature, chlorophyll a, nutrients, and sea-wind in the East/Japan Sea on the left- and right-hand sides of typhoon shanshan’s track

• Published in: Ocean science journal 2010, 45(4), , pp.253-265
• Main Authors: Lee, Chung Il, Park, Mi-Ok
• Format: Article
• Language: English
• Subjects: Aquatic Pollution; Earth and Environmental Science; Earth Sciences; Marine; Marine & Freshwater Sciences; Oceanography; Waste Water Technology; Water Management; Water Pollution Control; 해양학
• ISSN: 1738-5261; 2005-7172
• DOI: 10.1007/s12601-010-0023-2

Time series changes in sea surface temperature (SST), chlorophyll a (Chl a ), nutrients (PO 4 , NO 3 ), and sea winds, which correlated with the passage of Typhoon Shanshan in the East/Japan Sea (EJS), are illustrated using satellite data for Chl a , SST, sea winds, and in situ data for nutrients and water temperature. The sea-surface cooling (SSC) effect by the passage of the typhoon was higher at stations nearer to the center compared to stations further from the center. The SSC effect at stations in the colder water region (on the left side of the typhoon’s track) was higher than at stations in the Tsushima Warm Current region (on the right side of the typhoon). The SSC effect continued for approximately 10 days after the passage of the typhoon. The Chl a concentration at all stations increased after the passage of the typhoon. This increase continued for a period of approximately 10 days, but the duration period at each station varied with distance from the typhoon center. Changes in Chl concentrations at stations within a 2° distance on both sides from the typhoon’s center were higher than that at other stations. The changes in Chl a by the passage of the typhoon were measured at approximately 0.3–1.0 mg/m 3 along the moving path of the typhoon. Phosphate and nitrate changes were inversely correlated with the water temperature changes; the nutrient concentration increased with the passage of the typhoon. Like the changes in SST, changes in nutrient concentrations on the left side of the typhoon’s track were higher compared to those at the center and the right side.