[1]Wu Lixin, Li Chun. Causes and prediction of decadal climate variability[M]∥10000 Selected Problems in Sciences(Earth Science). Beijing: Science Press, 2010: 876-879.[吴立新, 李春. 气候年代际变化的成因及预测[M]∥10000 个科学难题(地球科学卷).北京:科学出版社, 2010: 876-879.]
[2]Liu Qinyu, Li Chun, Hu Ruijin. Interdecadal oscillations in the North Pacific and global warming[J]. Climatic and Enviromental Research, 2010, 15(2):217-224.[刘秦玉, 李春, 胡瑞金. 北太平洋的年代际振荡与全球变暖[J]. 气候与环境研究, 2010, 15(2):217-224.]
[3]Wu Lixin, Liu Zhengyu, Gallimore R, et al. Pacific decadal variability: The Tropical Pacific mode and the North Pacific mode[J]. Journal of Climate, 2003, 16(8): 1 101-1 120.
[4]Li Chun. Variation of Wind-driven Oceanic Gyre in the North Pacific and Its Feedback to Atmospheric Circulation[D]. Qingdao:Ocean University of China, 2010.[李春. 北太平洋风生环流变异及其对大气环流的反馈[D].青岛:中国海洋大学, 2010.]
[5]Li Chun, Wu Lixin. Dynamic linkage between the North Pacific and the Tropical Pacific: Atmosphere-ocean coupling[J]. Advances in Atmospheric Sciences, 2013, 30(2): 306-314.
[6]Li Chun, Wu Lixin, Xie Shangping. Impacts of interhemispheric asymmetric thermal forcing on tropical Pacific climate: Air-sea coupling and subduction[J]. Journal of Climate, 2013, 26(2): 575-582.
[7]Li Chun, Ma Hao. Coupled Modes of precipitation over China and the Pacific sea surface temperature in boreal summertime[J]. Advances in Atmospheric Sciences, 2011, 28(5): 1 201-1 214.
[8]Li Chun, Wu Lixin, Chang Ping. A far-reaching footprint of Tropical Pacific meridional mode on the summer rainfall over the Yellow River loop[J]. Journal of Climate,2011, 24(10): 2 585-2 598.
[9]Li Chun, Ma Hao. Relationship between ENSO and winter rainfall over Southeast China and its decadal variability[J]. Advances in Atmospheric Sciences, 2012, 29(6): 1 129-1 141.
[10]Li Chun, Gang Zeng. Impacts of ENSO on autumn rainfall over Yellow River loop valley in observation: Possible mechanism and stability[J]. Journal of Geophysical Research Atmospheres, 2013, 118(8):3 110-3 119. |