supported by National Natural Science Foundation of China(Grant No.42141017);National Basic Research Program of China(Grant No.2020YFA0608904);the National Natural Science Foundation of China(Grant Nos.41975112,42175142,42175013,and 41630532).
Since the 1950s,the terrestrial carbon uptake has been characterized by interannual variations,which are mainly determined by interannual variations in gross primary production(GPP).Using an ensemble of seven-member T...
supported by the National Basic Research Program of China (Grant Nos.2014CB953902,2011CB403505,and 2012CB417203);the Priority Research Program of the Chinese Academy of Sciences (Grant Nos.XDA11010402 and XDA01020302);the National Natural Science Foundation of China (Grant Nos.41175059 and 41375087)
Anomalous warming occurred in the equatorial central-eastern Pacific in early May 2014, attracting much attention to the possible occurrence of an extreme E1 Nifio event that year because of its similarity to the situ...
supported by the CAS Strategic Priority Project (the Western Pacific Ocean System: Structure, Dynamics and Consequences, WPOS);a China 973 project (Grant No. 2012CB956000);the Institute of Oceanology, Chinese Academy of Sciences (IOCAS);the National Natural Science Foundation of China (No. 41206017)
A hybrid coupled model (HCM) is constructed for El Nifio-Southern Oscillation (ENSO)-related modeling studies over almost the entire Pacific basin.An ocean general circulation model is coupled to a statistical atm...
supported by the National Natural Science Foundation of China (NSFC) (Grant Nos. 40975065 and 40821092);the National Basic Research Program (NBRP) "Ocean–atmosphere interaction over the joining area of Asia and the Indian-Pacific Ocean (AIPO) and its impact on the short-term climate variation in China" project(2006CB403605)
Using the Flexible Global Ocean-Atmosphere-Land System model (FGOALS) version g1.11, a group of seasonal hindcasting experiments were carried out. In order to investigate the potential predictability of sea surface ...
Supported by National Natural Science Foundation of China (Grant No. 40476017);the National Key Basic Research Projects (2006CB403605)
A common problem in the application of the coupled ocean-atmosphere general circulation models (CGCMs) without flux correction is that the simulated equatorial cold tongue in general tends to be too strong, narrow, ...