The impact of the ENSO on the winter monsoon in Taiwan
The East Asian region is influenced by the large low-level cyclonic and anticyclonic Asian monsoon circulation in summer and winter seasons, respectively. For most of the Asian monsoon regions such as South Asia, the summer monsoon season is referred to the “rainy season”, while the winter is usually a dry season. Over East Asia, there is a similar wet/dry and warm/cold monsoonal characteristics for the summer/winter season. However, the influence of the monsoon circulation in Taiwan is not exactly the same as this traditional point of view.
In northern Taiwan, the northerly and northeasterly flow of the East Asian winter monsoon (hereafter EAWM) can produce the orographic rain along the coastal regions during winter. In addition to this effect, the frontal activity is another source of rainfall for northern Taiwan during winter. Therefore, the wet/dry monsoonal characteristic is not fully applied in northern Taiwan. However, in southern Taiwan, this wet/dry monsoonal characteristic is clear. The major rainy season over there is during summer and the winter season is usually dry.
UAW今年將在韓國首爾召開。
http://ces.snu.ac.kr/uaw09/index.htm
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