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Comparison of impacts of intraseasonal oscillation on tropical cyclogenesis over the western North Pacific based on two methods 期刊论文
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2019
作者:  Cao, Xi;  Wu, Renguang
收藏  |  浏览/下载：6/0  |  提交时间：2019/11/27
GPI  ISO  relative contribution  TC genesis  the WNP  
Feedback of 10-20-day intraseasonal oscillations on seasonal mean SST in the tropical Western North Pacific during boreal spring through fall 期刊论文
CLIMATE DYNAMICS, 2018, 51: 4169-4184
作者:  Wu, Renguang
收藏  |  浏览/下载：4/0  |  提交时间：2019/04/09
ISO feedback  Seasonal mean SST  Latent heat flux decomposition  Tropical western North Pacific  
Summer Intraseasonal Surface Heat Flux-Sea Surface Temperature Relationship Over Northern Tropical Indo-Western Pacific in Climate Models 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2018, 123 (11) : 5859-5880
作者:  Wu, Renguang;  You, Ting
收藏  |  浏览/下载：0/0  |  提交时间：2019/04/09
boreal summer intraseasonal variations  surface heat flux-sea surface temperature relationship  the South China sea  climate model  
The impact of tropical intraseasonal oscillation on the summer rainfall increase over southern China around 1992/1993 期刊论文
CLIMATE DYNAMICS, 2017, 49
作者:  Wang, Jiabao;  Wen, Zhiping;  Wu, Renguang;  Lin, Ailan
收藏  |  浏览/下载：6/0  |  提交时间：2019/04/09
Intraseasonal oscillation (ISO)  Interdecadal change  Summer rainfall  Southern China  
Relationship of boreal summer 10-20-day and 30-60-day intraseasonal oscillation intensity over the tropical western North Pacific to tropical Indo-Pacific SST 期刊论文
CLIMATE DYNAMICS, 2017, 48 (11)
作者:  Wu, Renguang;  Cao, Xi
收藏  |  浏览/下载：3/0  |  提交时间：2019/04/09
ISO intensity variations  10-20-Day and 30-60-day ISOs  ENSO  The North Indian Ocean SST  Feedback of ISO intensity on SST  
Contrast of 10-20-day and 30-60-day intraseasonal SST propagation during summer and winter over the South China Sea and western North Pacific 期刊论文
CLIMATE DYNAMICS, 2017, 48
作者:  Cao, Xi;  Wu, Renguang;  Chen, Shangfeng
收藏  |  浏览/下载：3/0  |  提交时间：2019/04/09
Intraseasonal SST propagation  Surface heat flux contribution  Summer and winter  10-20-Day and 30-60-day time scales