supported by the National Basic Research Program of China (Grant No. 2012CB955602);the National Natural Science Foundation of China (Grant Nos. 41476002, 41490643, 41176006 and 41221063);the Fundamental Research Funds for the Central Universities (Grant No. 201503029)
The mixed layer is deep in January-April in the Kuroshio Extension region. This paper investigates the response in this region of mixed layer depth (MLD) and the spring bloom initiation to global warming using the o...
supported by the National Basic Research Program of China (Grant No. 2012CB955600);National Natural Science Foundation of China (Grant Nos. 41376009 and 41176006);Strategic Priority Research Program of the Chinese Academy of Sciences (Grant Nos. XDA11010302 and XDA11010201);the Joint Program of Shandong Province and National Natural Science Foundation of China (Grant No.U1406401)
Mode water is a distinct water mass characterized by a near vertical homogeneous layer or low potential vorticity, and is considered essential for understanding ocean climate variability. Based on the output of GFDL C...
supported by the National Basic Research Program of China(2012CB955602);Natural Science Foundation of China(41176006 and 41221063)
The responses of Sea Surface Temperature(SST) to greenhouse gas(GHG) and anthropogenic aerosol in the North Pa- cific are compared based on the historical single and all-forcing simulations with Geophysical Fluid Dyna...
supported by the National Basic Research Program of China(2012CB955603);the Natural Science Foundation of China(41106010,41176006);the 111 Project(B07036);the Qianren Program
Based on a coupled ocean-atmosphere model, the response of the Indian Ocean Dipole (IOD) mode to global warming is investigated with a six member ensemble of simulations for the period 1850-2100. The model can simulat...
supported by the National Basic Research Program of China(2012-CB955602);National Key Program for Developing Basic Science(2010CB428904);Natural Science Foundation of China(40830106,40921004 and 41176006)
Long-term change of sea surface temperature (SST) in the China Seas from 1900 to 2006 is examined based on two different observation datasets (HadlSSTI and HadSST3). Similar to the Atlantic, SST in the China Seas ...
supported by the Ministry of Science and Technology of China(National Basic Research Program of China(Grant No.2012CB955602));the National Key Program for Developing Basic Science(Grant No.2010CB428904);the Natural Science Foundation of China(Grant Nos.40830106,40921004,41176006)
A robust anomalous anticyclonic circulation (AAC) was observed over Northeast Asia and the Japan Sea in boreal win-ter 1997/98 and over the Japan Sea in spring 1998. The formation mechanism is investigated. On the bac...
supported by the National Basic Research Program of China(2012CB955602);National Key Program for Developing Basic Science(2010CB428904);Natural Science Foundation of China(41176006 and 40921004)
Six coupled general circulation models from the Coupled Model Intercomparison Project Phase 5 (CMIP5) are em-ployed for examining the full evolution of the North Pacific mode water and Subtropical Countercurrent (STCC...
supported by the National Basic Research Program of China(2012CB955602);National Key Program for Developing Basic Science(2010CB428904);Natural Science Foundation of China(41176006 and 40921004)
The response of the North Pacific Subtropical Mode Water and Subtropical Countercurrent (STCC) to changes in greenhouse gas (GHG) and aerosol is investigated based on the 20th-century historical and single-forcing sim...
supported by the National Basic Research Program of China 2012CB955602 and 2012CB955603;the Natural Science Foundation of China(41176006,40921004 and 41106010)
Seventeen coupled general circulation models from the Coupled Model Intercomparison Project Phase 5 (CMIP5) are employed to assess the relationships of interannual variations of sea surface temperature (SST) betwe...
supported by the National Basic Research Program of China(2012CB955602);Ministry of Science and Technology of China(National Key Program for Developing Basic Science 2010CB428904);the NSFC(41176006,40921004,41106010);the 111 Project of China(Program of Introducing Talents of Discipline to Universities No.B07036)
Using data from Argo and simple ocean data assimilation (SODA), the role of the barrier layer (BL) in the southeastern Arabian Sea (SEAS: 60°E-75°E, 0°-10°N) is investigated during the development of positive Indi...