首页|黄土高原次降雨径流产沙变化及其与雨强和植被盖度变化的相关性

黄土高原次降雨径流产沙变化及其与雨强和植被盖度变化的相关性

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获取12条流域16 a的753次降雨数据,运用雨强、植被盖度、径流系数和产沙系数等指标,分析黄土高原次降雨径流产沙变化及其与雨强和植被盖度变化的相关性.结果显示:①与1980-1989年相比,2006-2011年黄土高原的降雨—径流和径流—产沙关系发生了明显变化,大部分流域的产流产沙能力有所下降,10个流域中有8个流域的径流系数、产沙系数有所减小,分别减小25.93%~66.1%和59.05%~97.71%;②分析雨强和植被盖度变化与径流产沙变化的相关性,发现径流产沙变化与植被盖度变化的相关性强于其与雨强变化的相关性,表明植被盖度变化对径流产沙变化的影响更明显;③分析不同干湿条件下径流产沙变化对植被盖度变化的敏感性,发现气候越湿润,流域的径流产沙变化对植被盖度变化越敏感,植被改善的减水减沙效果越明显.
Changes in Event-Based Rainfall-Runoff-Sediment and the Relationships between These Changes and Rainfall Intensity and Vegetation Coverage Variations in Loess Plateau of China
It is important to analyze the changes in event-based rainfall-runoff-sediment and the relativities between these changes and rainfall intensity and vegetation coverage variations in the Loess Plateau of China for recognizing the causes of changes in water and sediment of the Yellow River.This study collected 753 event-based hydrological data of 16 years,12 watersheds located in the Loess Plateau of China,using four indicators,including rainfall intensity,vegetation coverage runoff coefficient,and sediment coefficient,and analyzed the changes in event-based rainfall-runoff-sediment and the relativities between these changes and rainfall intensity and vegetation coverage variations in the Loess Plateau of China.Results showed that:① the rainfall-runoff and runoff-sediment relationships changed significantly in the period from 2006 to 2011 compared to the period from 1980 to 1989,and the runoff and sediment generation capacities of most watersheds decreased.The runoff coefficient and sediment coefficient of eight in ten watersheds decreased 25.93%-66.1% and 59.05%-97.71%,respectively;② By analysing the relativities between rainfall intensity,vegetation coverage variations and runoff,sediment changes,we found that the vegetation coverage variation was stronger than rainfall intensity change related to the runoff and sediment changes,and it was indicated that the effect of vegetation coverage variation on runoff and sediment changes was more obvious;③) we also discussed the sensibilities of runoff and sediment yield changes on vegetation coverage variation in different dryness/wetness,and found that the wetter the climate,the more sensitive the variations of runoff and sediment yield on the change of vegetation coverage were,and the more obvious the reductions of runoff and sediment by vegetation improvement generated.

rainfall eventrunoffsediment yieldrainfall intensityvegetation coverageLoess Plateau of China

罗娅、杨胜天、刘晓燕、周秋文、董国涛

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遥感科学国家重点实验室,北京师范大学地理学与遥感科学学院,环境遥感与数字城市北京市重点实验室,北京100875

贵州师范大学地理与环境科学学院,贵州贵阳550001

黄河水利委员会,河南郑州450003

黄河水利科学研究院,河南郑州450003

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次降雨 径流 产沙 雨强 植被盖度 黄土高原

国家“十二五”科技支撑计划课题国家自然科学基金

2012BAB02B0041301496

2015

干旱区研究
中国科学院新疆生态与地理研究所 中国土壤学会

干旱区研究

CSTPCDCSCD北大核心
影响因子:1.157
ISSN:1001-4675
年,卷(期):2015.32(4)
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