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頁籤選單縮合
題名 | 臺灣梅雨季降雨氣候分析=An Analysis on the Rainfall Distribution during the Taiwan Mei-Yu Season |
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作者 | 陳來發; 鄭師中; Chen, Lai-fa; Cheng, Shih-chung; |
期刊 | 警專學報 |
出版日期 | 20000900 |
卷期 | 2:8 2000.09[民89.09] |
頁次 | 頁163-178 |
分類號 | 328.63 |
語文 | chi |
關鍵詞 | 梅雨季; 天氣類型; 雨量氣候; Mei-yu season; Weather pattern; Climate rainfall; |
中文摘要 | 臺灣地區每年五、六月受到梅雨鋒面影響,常發生豪(大)雨。本研究經由降雨之年際變化分析、各類綜觀天氣系統影響之降雨量分析,以及日雨量降雨強度之整合氣候分析,以了解臺灣梅雨季降雨之氣候特徵。結果顯示,臺灣各地區梅雨季總雨量年際變化相當大。另外就雨量分布的地理性差異而言,臺灣西半部及東半部的雨量差異頗大。西半部降雨的因素主要受到梅雨鋒面的影響,而影響東半部地區降雨的天氣系統較為多樣化。就降雨強度而言,六月份的降雨強度較五月份強,臺灣西半部較東半部強。 |
英文摘要 | During the May and June, the Mei-Yu fronts often bring heavy rainfall in Taiwan. The characteristics of the rainfall distribution are elucidatedby the analysis on the variation of yearly rainfall amount, the rainypatterns for synoptic weather system and the intensity of rainfall in thisstudy. The results show that the total rain in May and June around Taiwanis significantly various year by year. The spatial distribution of the rainfallin Taiwan depicts the local effect which is affected by the Central Mountain Ridge (CMR). On the western side of CMR, the rain is mostly caused by the Mei-Yu front, but on the other hand, it seems more complicated in the eastern side of CMR. According analysis of the intensity of daily rainfall, Juneis stronger than May, and western side of CMR is stronger than easternside. |
本系統之摘要資訊系依該期刊論文摘要之資訊為主。