中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
气候变化对渭河流域自然植被净初级生产力的影响研究(Ⅰ)——地表干湿状况时空演变特征分析

文献类型:期刊论文

作者蒋冲 ; 王飞 ; 穆兴民 ; 李锐
刊名干旱区资源与环境
出版日期2013
卷号27期号:04页码:30-07
关键词渭河流域 Wei river basin 湿润指数 humidity index Penman-Monteith模型 Penman - Monteith model 空间分布 spatial distribution 影响因素 extreme arid and
其他题名Effect of climate change on net primary productivity ( NPP) of natural vegetation
中文摘要采用1959~2010年23个气象站的逐日气象资料,利用FAO Penman-Monteith公式计算出渭河流域各气象站的潜在蒸散量,由此计算出各站的湿润指数。采用样条曲线插值法(Spline)、气候倾向率、标准化指数、相关分析等方法对流域湿润指数的时空变化特征以及影响其变化的气象要素进行了分析。结果表明:近52a渭河流域地表湿润指数整体下降,由南向北干旱程度逐渐增加。北部黄土高原丘陵沟壑区最干,南部秦岭山地和关中地区最湿。湿润指数年际间波动较大,与潜在蒸散量的变化趋势呈反相位关系,泾河和北洛河流域干湿分布规律与渭河流域整体类似。干旱化速率较大的为华山和宝鸡,关中部分地区微弱变湿。流域整体在春季和秋季变干,夏季除关中和陇东部分地区外也逐渐变干,冬季呈变湿趋势。影响湿润指数的因素主要为降水(正相关)和温度(负相关),风速的增加也会加剧干旱化的趋势
英文摘要Based on the daily data of 23 meteorological stations from 1959 to 2010,the potential evaporation
( ET0
) was calculated using the Food and Agriculture Organization ( FAO) Penman - Monteith model,and then
the humid index in the Wei river basin was reconstructed from the ET0 . With the method of spline interpolation,
climatic trend rate,normalized ratio and correlation analysis,etc,the temporal and spatial variations of humid
index and extreme arid and wet event,as well as its influential factors were discussed. The results indicated that
the humid index decreased in the last 52 years,drought phenomenon increased gradually from south to North,
with the driest condition in the loess hilly gully region and the wettest condition in Guanzhong Region and Qin
Mountain. The inter annual fluctuations of humid index was very significant and change trend of extreme points
presented a antiphase relation corresponding to the potential evaporation. Jing River and North Luo River had the
similar dry - wet condition to Wei River Basin. Drying rate was larger for the Hua Mountain and Baoji,
Guanzhong Region presented a trend of becoming wet. There was a positive correlation with precipitation and relative
humidity,and negative correlation with sunshine duration,potential evaporation and wind speed.
公开日期2014-10-20
源URL[http://ir.iswc.ac.cn/handle/361005/5562]  
专题水土保持研究所_水保所知识产出(1956-2013)
推荐引用方式
GB/T 7714
蒋冲,王飞,穆兴民,等. 气候变化对渭河流域自然植被净初级生产力的影响研究(Ⅰ)——地表干湿状况时空演变特征分析[J]. 干旱区资源与环境,2013,27(04):30-07.
APA 蒋冲,王飞,穆兴民,&李锐.(2013).气候变化对渭河流域自然植被净初级生产力的影响研究(Ⅰ)——地表干湿状况时空演变特征分析.干旱区资源与环境,27(04),30-07.
MLA 蒋冲,et al."气候变化对渭河流域自然植被净初级生产力的影响研究(Ⅰ)——地表干湿状况时空演变特征分析".干旱区资源与环境 27.04(2013):30-07.

入库方式: OAI收割

来源:水土保持研究所

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