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Role of the oceanic channel in the relationships between the basin/dipole mode of SST anomalies in the tropical Indian Ocean and ENSO transition 期刊论文
ADVANCES IN ATMOSPHERIC SCIENCES, 2016, 卷号: 33, 期号: 12, 页码: 1386-1400
作者:  Zhao, Xia;  Yuan, Dongliang;  Yang, Guang;  Zhou, Hui;  Wang, Jing
Adobe PDF(7013Kb)  |  收藏  |  浏览/下载：268/0  |  提交时间：2017/03/21
Indian Ocean Sstas  Dipole Mode  Basin Mode  Enso Transition  Oceanic Channel  
Testing a four-dimensional variational data assimilation method using an improved intermediate coupled model for ENSO analysis and prediction 期刊论文
ADVANCES IN ATMOSPHERIC SCIENCES, 2016, 卷号: 33, 期号: 7, 页码: 875-888
作者:  Gao, Chuan;  Wu, Xinrong;  Zhang, Rong-Hua
Adobe PDF(1168Kb)  |  收藏  |  浏览/下载：314/0  |  提交时间：2016/09/21
Four-dimensional Variational Data Assimilation  Intermediate Coupled Model  Twin Experiment  Enso Prediction  
Assessment of Interannual Sea Surface Salinity Variability and Its Effects on the Barrier Layer in the Equatorial Pacific Using BNU-ESM 期刊论文
ADVANCES IN ATMOSPHERIC SCIENCES, 2016, 卷号: 33, 期号: 3, 页码: 339-351
作者:  Zhi, Hai;  Zhang, Rong-Hua;  Zheng, Fei;  Lin, Pengfei;  Wang, Lanning;  Yu, Peng
Adobe PDF(6781Kb)  |  收藏  |  浏览/下载：325/0  |  提交时间：2016/05/03
Feedback  Interannual Variability  Sea Surface Salinity  Barrier Layer Thickness  
A Global Spectral Element Model for Poisson Equations and Advective Flow over a Sphere 期刊论文
ADVANCES IN ATMOSPHERIC SCIENCES, 2016, 卷号: 33, 期号: 3, 页码: 377-390
作者:  Mei, Huan;  Wang, Faming;  Zeng, Zhong;  Qiu, Zhouhua;  Yin, Linmao;  Li, Liang
Adobe PDF(2474Kb)  |  收藏  |  浏览/下载：190/0  |  提交时间：2016/05/03
Spectral Element Method  Spherical Coordinates  Poisson Equations  Advective Equation  Legendre-gauss-radau  
Weak ENSO Asymmetry Due to Weak Nonlinear Air-Sea Interaction in CMIP5 Climate Models 期刊论文
ADVANCES IN ATMOSPHERIC SCIENCES, 2016, 卷号: 33, 期号: 3, 页码: 352-364
作者:  Sun, Yan;  Wang, Fan;  Sun, De-Zheng
Adobe PDF(64Kb)  |  收藏  |  浏览/下载：234/1  |  提交时间：2016/05/03
Enso Asymmetry  Nonlinearity  Air-sea Interaction  Cold Tongue  Cmip5  Deep Convection