近十年台灣降雨沖蝕指數之時空分布
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摘要
近年来因极端降雨事件发生频繁,造成降雨型态产生明显的改变,导致通用土壤流失公式(universal soil loss equation,USLE)中的降雨冲蚀指數(rainfall erosivity index,R)亦随之改变,间接影响土壤冲蚀量的估算。目前台湾地区降雨冲蚀指数大多以黄俊德(1979)建立的台湾年平均降雨冲蚀指数等值图。于2000年后迄今,若计算降雨冲蚀指数仍沿用黄俊德(1979)的结果,可能有部分地区产生低估现象,故有必要重新订定(俞俊宾,2008)。因此,本研究以全台湾为研究区域,搜集区域内293个雨量站2002-2012年的10分钟雨量数据,进行降雨冲蚀指数的分析,回归出台湾各区之年降雨量及降雨冲蚀指数之关系式,并利用ArcGIS绘制台湾年平均降雨冲蚀指数等值图,如图1所示。而在降雨冲蚀指数时间变化部分,本研究搜集台北(北)、日月潭(中)、高雄(南)及花莲(东)4个气候站之历年年雨量资料,带入本研究之年降雨量及降雨冲蚀指数关系式,计算4个气候站之年平均降雨冲蚀指数,并绘制年降雨量及年降雨冲蚀指数之变化趋势图。研究结果显示,区域内293个雨量站2002-2012年的有效降雨事件共108,124场。年平均降雨冲蚀指数图之变化范围在5,000~70,000 MJ-mm/ha-hr-yr,最大值发生在御油山雨量站为78,772 MJ-mm/ha-hr-yr,其较大值多集中于中央山脉西南部一带。另外,由气候站降雨量及降雨冲蚀指数之变化趋势图可知,台湾之北、中、南及东部4个区域,其年降雨量及年降雨冲蚀指数皆有逐年上升趋势,其中以北部及东部较为明显。本研究成果可提供水土保持相关规划工作之参考依据。
Global climate change can modify rainfall patterns,leading to more extremes with associated erosion events.Rainfall erosivity(R-factor) based on the Universal Soil Loss Equation(USLE).This study used 293 rainfall stations with short-term 10-min rainfall data from 2002 to 2012(108,124 storm events),and 4rainfall stations with long- term annual rainfall data of over 30 year.The annual R- factor in Taiwan was classified as medium-strong and strong erosivity,which represented a range from 5,000 to 70,000 MJ-mm/ha-hr-yr.The maximum annual R-factor value of 78,772 MJ-mm/ha-hr-yr was observed at the YuYouShan station.A simple power relation between annual R-factor and annual rainfall was derived.The long-term change trend analysis showed significant increasing trend observed in northern and eastern Taiwan.The result provided a reference for land-use planner and agriculture management in Taiwan.
引文
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