【Time】: 2016-7-25 (星期一) 11:40-13:30(12:20开始讲座)
【Count】: 1146 【Updated on】: 2016-7-21 |
【Venue】:
1F Multifunctional Hall, Zhou Long Quan Bldg |
【Speaker】:
Prof. Leo Oey |
【Institution】: National Central University |
【Host】: Dr. Yuwu Jiang
【Contact】: Vera Shi, vera_shiwei@xmu.edu.cn |
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Abstract:
I will use independent storm surge and precipitation data to argue that the answer is affirmative. I will then explore the possibility that the cause is related to the continued weakening of the large-scale steering flow over the western Pacific, which in turn is connected to rising SLP over the maritime continent consistent with a general slow-down of the tropical atmospheric overturning circulation due to climate warming.
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