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How do the northeast monsoon and typhoon wind speed influence each other in terms of storm surge? 


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The interaction between the northeast monsoon and typhoon wind speed significantly impacts storm surge. Research shows that non-stationarity exists in both typhoon and monsoon wind speeds, with stronger non-stationarity in typhoon wind speed . Typhoon intensity factors, such as maximum wind speed and translation speed, play a crucial role in storm surge generation, with storm surge showing a positive correlation with the distance of the typhoon's center . Additionally, the size of a typhoon, represented by the radius of the maximum wind, influences peak storm surge height, with larger typhoons leading to higher surge heights, especially in semi-enclosed areas like Tokyo Bay . Understanding these dynamics is essential for accurate storm surge forecasting and disaster mitigation efforts.

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The northeast monsoon and typhoon wind speed can interact, affecting storm surge. Higher typhoon wind speeds generally lead to more significant storm surge impacts in the Northern East China Sea.
The northeast monsoon and typhoon wind speed interact to influence storm surge severity, with storm surge inundation being modulated by typhoon intensities and tracks.

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