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Wei-Ting Chen, Shih-Pei Hsu, Yuan-Huai Tsai, and Chung-Hsiung Sui

MSLP requirement and exhibited northeasterly conditions, but the areal mean wind speed was only around 6 m s −1 , indicating moderate events of a cold air outbreak. Therefore the tropical–extratropical interaction associated with the East Asian cold surge was not significant during this month. 4. Convectively coupled tropical waves in December 2016 a. Kelvin waves Figure 3a shows the Hovmöller diagram of total OLR and 925-hPa zonal wind from the IO to the WP in the equatorial band (5°S–5°N) during

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Dipanjan Chaudhuri, Debasis Sengupta, Eric D’Asaro, R. Venkatesan, and M. Ravichandran

( Frank and Husain 1971 ; Webster 2008 ). Communities living around the large river deltas of India, Bangladesh, and Myanmar are particularly vulnerable to storm surge and flooding from cyclones (e.g., De et al. 2005 ; Raghavan and Rajesh 2003 ; Adler 2005 ; Lin et al. 2009 ). The BoB experiences an average of three to four tropical cyclones per year; there are two cyclone seasons, April–June and late September–December (premonsoon and postmonsoon seasons). The temperature–salinity structure of

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