globalchange  > 气候变化与战略
CSCD记录号: CSCD:5331331
论文题名:
近50年秦岭南北≥0 ℃热量资源的时空分布规律
其他题名: Patiotemporal distribution of thermal resources over northern and southern regions of the Qinling Mountains in recent 50 years
作者: 高蓓1; 卫海燕1; 郭彦龙1; 董金芳2
刊名: 中国农业大学学报
ISSN: 1007-4333
出版年: 2015
卷: 20, 期:1, 页码:1798-1804
语种: 中文
中文关键词: ≥0 ℃热量资源 ; 秦岭地区 ; 时空变化 ; 统计分析
英文关键词: ArcGIS ; thermal resources of daily average temperature above 0 ℃ ; Qinling Mountains ; spatial-temporal variation ; statistic analysis ; ArcGIS
WOS学科分类: METEOROLOGY ATMOSPHERIC SCIENCES
WOS研究方向: Meteorology & Atmospheric Sciences
中文摘要: 为向全球变暖背景下的陕西省秦岭地区生态环境建设和区域农业发展提供科学依据,采集19612010年该区域71个气象台站的资料,采用气象数据小网格推算、Mann-kendall突变检验、Morlet小波分析法,分析了秦岭南北近50年来稳定通过≥0 ℃的热量资源的积温、初日、终日和持续日数的变化特征,结果表明:近50年来秦岭南北≥0 ℃的积温增加、初日提前、终日推迟和持续日数延长,除秦岭北部≥0 ℃初日变化速度慢于秦岭南部外,秦岭北部≥0 ℃的积温、终日和持续时间变化速度快于秦岭南部;秦岭南北≥0 ℃的积温和持续日数发生由少到多突变的年份分别为2003和1997年,秦岭南北≥0 ℃初日发生由推迟到提前的突变年份为1997年,秦岭南北≥0 ℃终日发生由提前到推迟的突变年份为1972和1976年。秦岭地区≥0 ℃积温的空间变化相似,整体呈增加趋势。秦岭南北初日和持续日数具有相同的周期,秦岭南北的终日具有相同的短周期,而秦岭南北的积温具有相同的长周期。
英文摘要: Under the background of global warming,in order to provide scientific basis for ecological environment construction and regional agricultural development of Qinling Mountains in Shaanxi. Based on the daily average temperature data collected from 71 weather stations in Qinling Mountains from 1961 to 2010, the methods like meteorological data of spatial analysis, Mann-kendall and Morelt wavelet analysis are used to analyze the thermal resources variation of accumulative temperature, interval days, first day and last day, with which daily temperature steadily above 0 ℃. The aim was to provide scientific evidence for the regional ecological environmental construction and agriculture development. The results showed that the interval days and accumulated temperature of the daily temperature above 0 ℃ steadily increased. The first day was early, but the last day was delayed. In addition, the changing speed of the first day in the northern Qinling mountain was slower than that of the southern region. The rate of the internal days, last day and accumulative temperature of daily temperature above 0 ℃ in northern Qingling mountains were quicker than those in southern area. Variation of the internal days, last day and accumulated temperature of daily temperature above 0 ℃ in Northern Qinling Mountain were higher than those of South part. However,the first day of daily temperature above 0 ℃ in Northern Qinling Mountain was lower than that of south. The abrupt change of the internal days,accumulated temperature, first day and last day of daily temperature above 0 ℃ in Northern Qinling Mountain appeared in 1997,1997,1972 and 1997 respectively. In contrast, they appeared in 2003,1997,1976 and 1997 respectively in Southern Qinling Mountain. The accumulated temperature of ≥0 ℃ in Qinling Mountain had similar spatial variation and increasing trend.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/150244
Appears in Collections:气候变化与战略

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作者单位: 1.陕西师范大学旅游与环境学院, 西安, 陕西 710062, 中国
2.陕西省农业遥感信息中心, 西安, 陕西 710015, 中国

Recommended Citation:
高蓓,卫海燕,郭彦龙,等. 近50年秦岭南北≥0 ℃热量资源的时空分布规律[J]. 中国农业大学学报,2015-01-01,20(1):1798-1804
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