Kuroshio

Kuroshio is a strong western boundary current. And the source area of Kuroshio has always been a very hot topic for oceanographers.

The place of the Kuroshio entering into the continental shelf is always at the northeast area of Taiwan.

The powerful Kuroshio shoots warm water northward, allowing coral reefs to thrive where they would not normally be found.

The source of the Yellow Sea Warm Current in the bottom layer is mixed by water of the Kuroshio and some current from the continental shelf.

during the winter dry season , the kuroshio oceanic current brings warm water of high salinity from the pacific through the luzon strait.

Theirconveyor belt was the Kuroshio (Black) Current, named after the deep colour of its waters.

This bending of the Kuroshio favors the formation of the anticyclone eddy in the east of the Luzon strait.

The results show that Kuroshio deformation takes the perpetual shape of'loop'in Luzon Strait.

By use of the observational and numerical methods, the interaction of Kuroshio SSTA and the East Asian monsoon are studied in this paper.

The selection of level of no motion is a basic problem in calculating the geostrophic flow in the East China Sea Kuroshio area.

Results reveal that the Kuroshio upper layer temperature experienced slight rise while salinity decreased in the past 50 years.

When the north transport of Kuroshio is large, the west transport through Luzon Strait is small.

Under 50m, Kuroshio is the main resource of the Taiwan warm current.

the Kuroshio front meander and the Kuroshio path meander.

The results show that: the SCS branch of the Kuroshio Current is an important part in the north SCS from Jan. to Aug.

In addition, Kuroshio plays a significant role in the enrichment of Fe-Mn micro-nodules.

Okinawa Churaumi Aquarium, as has the world's third largest water tank, "Kuroshio Sea, " is famous, 7, 500 tons of water tank.

In autumn and winter, the main intrusion of the Kuroshio happens in the surface and mid layers;

Numerical Simulation of the Influence of Successively Anomalous Winter Wind Field on Ocean Currents around the Kuroshio Area

Annual Variation of the Kuroshio Transport in a Two-Layer Numerical Model with a Ridge

Observation of frontal waves and associated salinity minimum formation along the Kuroshio Extension

Cooperative Study of the Kuroshio and Adjacent Regions

Numerical Simulations on the Influence of the Previous Winter Kuroshio SSTA on East Asian Summer Monsoon

Study on Circulation Substructure in the Main Part of the Kuroshio in the East China Sea

Application of nonlinear conjugate gradient method in geostrophic velocity calculation of Kuroshio in the East China Sea

Structure of the Temperature in the Northern South China Sea, During the Anticyclonic Eddy Shedding from the Kuroshio Bend

Some Phenomena of the Kuroshio Intrusion Into Shelf Area and the Shelf Circulation of the East China Sea

Numerical study on the Kuroshio path states in the northern Okinawa Trough of the East China Sea

Numerical simulation of Kuroshio circulation

Study on biodiversity of zooplankton in the Kuroshio in the north of the East China Sea

Relationship between Autumn Kuroshio SST and East Asian Winter Monsoon

Effect of Sea-bottom Undulation on Sound Propagation on PN Section in the East China Sea Kuroshio A

Effects of Topography on Kuroshio Frontal Meanders in the East China Sea

Climatological simulation of Kuroshio in the East China Sea

Water Mass Analysis of the Source Area of Kuroshio

Fig. 7 Heat transport tO east china sea by Kuroshio and total surface heat flux of East China Sea