globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6312498
论文题名:
近55 a渭河流域气候变化
其他题名: Climate change characteristics in Weihe River Basin from 1960 to 2015
作者: 冯星; 郭建青; 孙东永; 曹洋
刊名: 干旱区地理
ISSN: 1000-6060
出版年: 2018
卷: 41, 期:4, 页码:718-725
语种: 中文
中文关键词: 渭河流域 ; 气候特征 ; 极端干旱事件 ; Penman-Monteith模型
英文关键词: Weihe River Basin ; climatic characteristics ; extreme drought events ; Penman-Monteith model
WOS学科分类: METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向: Meteorology & Atmospheric Sciences
中文摘要: 利用渭河流域21个气象站点19602015年逐日气象资料,应用一元线性趋势分析、Penman- Monteith模型和Morlet小波分析等技术手段分别研究年、月地表湿润指数,并对其进行标准化和气温、降水以及极端干旱事件的变化趋势计算,并分析年内变化规律,以期更好的揭示渭河流域近55 a气候的变化规律。结果表明:(1)渭河流域近55 a的气温总体上在波动中呈小幅增加的趋势,其中20世纪80年代中期到90年代初期气温的增长幅度较大,为气温升高的主要时期,年均降水量和极端干旱频率呈现小幅减少的趋势,下降的主要时期集中在80年代中后期到90年代初期和21世纪初。(2)小波周期分析发现渭河流域极端干旱事件的震荡周期尺度为13~ 15 a和25~ 30 a,气温震荡周期的时间尺度为13~ 15 a和25~ 30 a,年降水量的小波振荡周期为15~ 17 a和25~ 30 a。主震荡周期的时间尺度均为25~ 30 a,次震荡周期的时间尺度也较为接近,为13~ 15 a和15~ 17 a,说明三者的变化规律在一定程度上有一定的相似性。(3)研究区内5个区域的气候变化特征同时存在着一定的差异性,天水西吉流域的年均降水量和极端干旱事件发生频率的减少幅度和年均气温的增加幅度是5个区域里变化最大的,吴其状头区域的年均降水量和极端干旱事件的减少频率和年均温度的增加频率是5个区域里变化幅度最小的,但在总体上各区域气候要素变化趋势上是保持一致的。
英文摘要: According to the daily meteorological data of 21 stations from 1960 to 2015 in Weihe River Basin, northwest China,We used Penman-Monteith model,climate inclination rate and Morlet wavelet to study the characteristics of climate change in Weihe River basin. The results showed as follows: (1) Annual temperature was in a slowly rising trend in recent 55 years,in particular,the rate of temperature rising from the middle of the 1980s to the early 1990s was faster than the rate at any other times. The annual precipitation has been slowly declined in recent 55 years. The periods from the middle of the 1980s to the early 1990s and the early 21st century were the major precipitation decreased periods. (2) The results from Morlet wavelet analysis indicated a vibration period scale as 13 years to 15 years for a sub fluctuation and 25 years to 30 years for a main fluctuation about both the extreme drought events and the air temperature,a sub fluctuation of 15 years to 17 years and main fluctuation of 25 years to 30 years about the annual precipitation. It is shown that the changing rules of the three are similar. (3) There are some differences in the climate change characteristics of the research area. The minimal trend of the annual temperature and precipitation is Wuqi-Zhuangtou Basin,and the greatest change trend of annual precipitation and extreme drought events is Tianshui-Xiji Basin. In general,the change of climate elements in the research area are basically consistent.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/157756
Appears in Collections:气候变化事实与影响

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作者单位: 长安大学, 旱区地下水文与生态效应教育部重点实验室, 西安, 陕西 710054, 中国

Recommended Citation:
冯星,郭建青,孙东永,等. 近55 a渭河流域气候变化[J]. 干旱区地理,2018-01-01,41(4):718-725
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