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논문 상세정보

2000년 5월 제주도 주변해역의 해황 및 표층 저염분수의 출현

Oceanographic Conditions in the Neighboring Seas of Cheju Island and the Appearance of Low Salinity Surface Water in May 2000

Abstract

In the adjacent seas of Cheju Island, the oceanographic conditions show low salinity surface waters starting in May. This water flows from the southeast part of the China Coastal Water, which flows southeastward along the Great Yangtze Sand Bank until April, with the help of southeasterly winds and flows from the adjacent sea off Cheju Island. In May, the Tsushima Warm Current and the low salinity surface water fluctuate in short and long-term periods as influenced by Yellow Sea Cold Water, which flows to the bottom layer at the western entrance of Cheju Strait. Temperature and salinity fronts in the northeastern sea area of U Island are formed in the boundary area between the Tsushima Warm Current, which expands towards Cheju Island from the southeastern sea area of Cheju Island and Hows out from the eastern entrance of the strait. Seasonally, additional oceanographic conditions, such as coastal counter-currents, which flow southward, appears within limited areas in the adjacent eastern and western seas of Cheju Island.

저자의 다른 논문

참고문헌 (17)

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이 논문을 인용한 문헌 (1)

  1. 2009. "" Ocean science journal : OSJ, 44(1): 1~10 

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