October 25,2024 marks the centennial anniversary of the Ocean University of China.The predecessor,Qingdao University,was established in 1924 as a private university,before it became a public university in 1928,and ren...October 25,2024 marks the centennial anniversary of the Ocean University of China.The predecessor,Qingdao University,was established in 1924 as a private university,before it became a public university in 1928,and renamed as National Shandong University in 1932.The centennial anniversary is a testament to the university’s special significance and mission in China’s ocean science.展开更多
The Indian Ocean Dipole (IOD) is an intrinsic ocean-atmosphere coupled mode in the tropical Indian Ocean (IO)[1,2]. It features a sea surface temperature (SST) anomaly gradient, defined by the dipole mode index (DMI),...The Indian Ocean Dipole (IOD) is an intrinsic ocean-atmosphere coupled mode in the tropical Indian Ocean (IO)[1,2]. It features a sea surface temperature (SST) anomaly gradient, defined by the dipole mode index (DMI), the difference of area-averaged SST anomaly between the western tropical IO (50°–70°E, 10°N–10°S)and the southeastern tropical IO (90°–110°E, Eq.-10°S). The IOD event tends to develop and mature in the boreal summer and fall seasons. When a positive IOD (p IOD) occurs, SST warms up in the west and cools down in the east, which sets up an east-west pressure gradient. The atmosphere hence responds to the展开更多
文摘October 25,2024 marks the centennial anniversary of the Ocean University of China.The predecessor,Qingdao University,was established in 1924 as a private university,before it became a public university in 1928,and renamed as National Shandong University in 1932.The centennial anniversary is a testament to the university’s special significance and mission in China’s ocean science.
基金supported by the National Key Research and Development Program of China(2022YFE0106400)the National Natural Science Foundation of China(42122039)special funds from Shandong Province for Qingdao Marine Science and Technology National Laboratory(2022QNLM010203)。
基金supported by the National Key Research and Development Program of China (2018YFA0605700)supported by the Joint Research Centre for Southern Hemisphere Oceans Research (CSHOR)between the Qingdao National Laboratory for Marine Science and Technology (QNLM)and the Commonwealth Scientific and Industrial Research Organisation (CSIRO)+10 种基金supported by the Australian Research Council Special Research Initiative for Securing Antarctica’s Environmental Future (SR200100005)supported by the National Natural Science Foundation of China (41876231)supported by the National Natural Science Foundation of China (42230405 and 41976006)the National Natural Science Foundation of China (41876008 and 41730534)supported by the National Natural Science Foundation of China (41830538)the Program of Impact and Response of Antarctic Seas to Climate Change (IRASCC 01-01-01A)supported by the National Key Research and Development Program of China (2020YFA0608801)the Youth Innovation Promotion Association of Chinese Academy of Sciences (2021205)supported by the National Science Foundation (AGS-1934392)supported by the National Science Foundation (OCE-2048336)the International Partnership Program of Chinese Academy of Sciences (183311KYSB20200015)。
基金supported by the State Oceanic Administration of China (GASI-IPOVAI-02)the National Natural Science Foundation of China (41525019, 41521005)+3 种基金the Strategic Priority Research Program of the Chinese Academy of Sciences (XDA11010103)the National Basic Research Program of China (2018YFA0605704)supported by a joint research Centre for Southern Hemisphere Ocean Research (CSHOR) between QNLM and CSIROsponsored by NASA Earth Science funding, available at www.remss.com
文摘The Indian Ocean Dipole (IOD) is an intrinsic ocean-atmosphere coupled mode in the tropical Indian Ocean (IO)[1,2]. It features a sea surface temperature (SST) anomaly gradient, defined by the dipole mode index (DMI), the difference of area-averaged SST anomaly between the western tropical IO (50°–70°E, 10°N–10°S)and the southeastern tropical IO (90°–110°E, Eq.-10°S). The IOD event tends to develop and mature in the boreal summer and fall seasons. When a positive IOD (p IOD) occurs, SST warms up in the west and cools down in the east, which sets up an east-west pressure gradient. The atmosphere hence responds to the
