Study results indicate that hyetograph using Huff method has an undulate shape and the smallest sum of square error, however the peak and the time to peak are not representative.

 
  • 主要成果如后述如:無(wú)因次平均法雨型曲線(xiàn)變化較為緩和,以致尖峰降雨時(shí)間及尖峰降雨量無(wú)法適切模擬;但對于分析同一集水區內不同雨量站之變化與降雨資料的呈現,無(wú)因次平均法為一不錯的選擇。
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