The data used in this paper include daily catches of Ommastrephes bartrami during 1995 to 2002 by Chinese fishing boats, SST isoline charts from 1991 to 2001 issued by Japan Fisher Information Service Center in the interval of every 3 days, the Kuroshio path charts and temperature isoline charts on 0m, 100m, 200m depths from 1998 to 2003 issued by Japan Coast Guard in 15-day span.

Climatological simulation of Kuroshio in the East China Sea;

Dynamics of eddy-induced Kuroshio variability in Luzon Strait;

Relationship Between the Kuroshio Temperature and Salinity in the East China Sea and the Air Temperature and Precipitation in the East China;

Responses of Sea Surface Temperature and Productivity to the Changes of the Kuroshio Current in the Northern Okinawa Trough during the Holocene

The sedimentological records of the evolution of the Kuroshio Current have been compared directly with the historical and archaeological data of the paleoenvironmental changes in the Yangtze River Mouth in this study.

Using POM 97, an oceanic mode, we separately do numerical tests tosimulate the 3-D structure of temperature in the sea area around Taiwan Island with orwithout the effect of Kuroshio Current.

The study of the temporal and spatial characteristics of western boundary current East of Ruykyu submarne ridge and the transport of Kuroshio in East China Sea;

Numerical Analysis of Kuroshio Chaos;

Using semidifferential stripping technique combined with pre-equibrium complex-ometric titration, the apparent copper complexing capacity (AXuCC) of seawater and the conditional formation constant (Kc) of copper-natural organic ligand of 65 seawater samples collected in the Kuroshio area in the East China Sea "in 1989 were determined.