supported by the National Natural Science Foundation of China (Nos. 41676004, 41506034, 41376001, 41376038, 41806123, 41430963);the Basic Scientific Fund for National Public Research Institutes of China (No. GY0213G02);the National Major Scientific Research Program (No. 2015CB954300);the National Science and Technology Major Project (No. 2016ZX05057015)
On the basis of the conductivity temperature depth(CTD)observation data off the coast of the Philippines(7.5°–18°N,130°E–the east coast of the Philippines)in the fall of 2005,the water mass distribution,geostroph...
Supported by the National Program on Global Change and Air-Sea Interaction(Nos.GASI-03-01-01-05,GASI-IPOVAI-01-02,GASIIPOVAI-02,GASI-IPOVAI-03,GASI-IPOVAI-01-05,GASI-03-01-01-02);the National Natural Science Foundation of China(Nos.41421005,41720104008,41476025,41376038,41206019);the Shandong Joint Fund for Marine Science Research Centers(Nos.U1606402,U1606405);the CAS Strategic Priority Project(No.XDA11010205);the Scientific and Technological Innovation Project of Qingdao National Laboratory for Marine Science and Technology(No.2016ASKJ04);the National Science and Technology Major Project(No.2016ZX05057015);the Open Fund of Shandong Provincial Key Laboratory of Marine Ecology and Environment&Disaster Prevention and Mitigation(No.201701)
A 1.5-layer quasi-geostrophic reduced gravity ocean circulation model is used to study the propagation of mesoscale eddies across a western boundary current(WBC) either leaping across or penetrating in an anti-cycloni...