Formation Processes of Intermediate and Deep Waters in the Okinawa Trough
Water mass formations in the intermediate and deep layers of the Okinawa Trough are investigated in connection with water mass distributions near the slope areas east of Taiwan and the Ryukyu Islands.We use two distinct datasets: a quasi-climatological salinity,potential temperature and depth dataset on the minimum salinity surface with a relatively high horizontal resolution (1/3°×1/3°),which was produced with Argo float profile data in addition to historical CTD data,and a velocity dataset below about 500 m depth in the Kerama Gap during 2009/06–2011/06,which was measured by moored current-meters.
Salinity minimum Interleaving Water exchange Hydraulic control Deep ventilation
Hirohiko Nakamura Ayako Nishina Fumiyo Tanaka Zhaojun Liu Mark Wimbush Jae-Hun Park
Faculty of Fisheries, Kagoshima University, Kagoshima, JAPAN Graduate School of Oceanography, University of Rhode Island, Rhode Island, USA Korea Institute of Ocean Science and Technology, Ansan, KOREA
国际会议
The 17th Pacific -Asian Marginal Seas Meeting(第十七届太平洋与亚洲边缘海国际会议)
杭州
英文
28-37
2013-04-23(万方平台首次上网日期,不代表论文的发表时间)