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• W3128587531 endingPage "101208" @default.
• W3128587531 startingPage "101208" @default.
• W3128587531 abstract "Tropical easterly waves are common features in the trade wind zones and they are important sources of tropical cyclogenesis. Despite numerous studies have analyzed the genesis and maintenance of easterly waves in the Western North Pacific, few had examined their dissipation processes. Focusing on tropical easterly waves during May-September of 1979–2017, this study shows that most of the easterly waves (∼70 %) eventually dissipate when encountering the monsoon trough and associated westerlies, while 22 % were carried northward by the monsoonal southwesterly flows and became recurving disturbances. Less than 10 % of easterly waves propagate across the South China Sea against the prevailing monsoon westerlies and into the Indochina peninsula. The vorticity budget analysis illustrates that total vortex stretching in the lower troposphere is the key factor in propelling the small number of easterly waves westward, suggesting that stronger and more convectively active easterly waves tend to move further into the developed monsoon trough. This echoes the previous observation that tropical disturbances alone have a limited probability in developing into a typhoon, for those disturbances or easterly waves almost always need to interact with the monsoon trough or a monsoon gyre, as well as other intraseasonal features to sustain the organized convection and rotation." @default.
• W3128587531 created "2021-02-15" @default.
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• W3128587531 date "2021-03-01" @default.
• W3128587531 modified "2023-10-14" @default.
• W3128587531 title "Dissipation process of summer tropical easterly waves in Western North Pacific" @default.
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• W3128587531 doi "https://doi.org/10.1016/j.dynatmoce.2021.101208" @default.
• W3128587531 hasPublicationYear "2021" @default.
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