臺灣的日雨量及雨日延遲特性
Rainfall is created by the interaction between the earth surface and its atmospheric layer through different scales of time and space. Some suggest that it is better to treat rainfall process in discrete time series，while most researchers prefer continuous probability density functions in describing rainfall data. Both continuous and discrete characters，depending upon the chosen methodology，can be observed. Coding the time stream with rain/non-rain，we have the rhythms of weather spells across space. Assigning every raining unit of time-space the rainfall amount to build up the distribution of rainfall density，we have the spectrum of rainfall across the earth surface. It is，then，lead to Kirkby”s statement on the convolution of the rainfall and the drainage network in producing the hydrological response at hydro-gauge.
台湾地区 日雨量 雨日延迟特性
雷鴻飛
Department of Geography,Chinese Culture University
国内会议
2007年全球华人地理学家大会暨2007海峡两岸地理学家大会——中国地理学会年度研究生联合论文发表会
台湾高雄
中文
179-185
2007-04-28（万方平台首次上网日期，不代表论文的发表时间）