On the basis of NOAA satellite MCSST image, we found that the mesoscale warm eddy produced by Kuroshio flow into the East China Sea has remarkable effect of modulation on upwelling.

Satellite altimetry data were used to determine the locations, scales and life-spans of the mesoscale eddy A and B, respectively.

Observation of mesoscale eddy fields in the sea southwest of Taiwan by TOPEX/POSEIDON altimeter data;

Variability of the Kuroshio in the East China Sea and the currents east of Ryukyu Islands Ⅱ.Variability of the currents and the meso-scale eddies in the region southeast of Okinawa Island;

The sea level anomaly (SLA) and mesoscale eddies during the period from 1993 through 2004 in the Kuroshio extension region(120oE-170oE, 25oN-45oN) and South China Sea(105oE-121oE, 0oN-25oN) are analyzed using altimetry data from CNES detected by TP/Jason-1 and ERS/ENVISAT.

The effects of oceanic structure variability caused by ocean mesoscale features(such as mesoscale eddies and fronts) on sound propagation are studied and two mesoscale feature oceanic environment models are.

By performing eight experiments with a high resolution barotropic model,which is integrated for 36 hours,the interaction between a mesoscale vortex and a typhoon vortex is investigated with its effect on the variation of typhoon intensity.

ased on observational data and a mesoscale numerical model (MM4), the numeric simulational results of a deep mesoscale vortex at high level which related to a heavy rain event are presented.

The rising branch of the Jet secondary circulation resulted in a surface mesoscale vortex.

The analysis suggests that the heavy rain event was close related to the generation and development of a mesoscale vortex in the mid-low troposphere.