生态与农村环境学报 ›› 2015, Vol. 31 ›› Issue (1): 30-38.doi: 10.11934/j.issn.1673-4831.2015.01.005

• 区域环境与发展 • 上一篇    下一篇

陕西商州近60 a极端气温变化

李如意, 赵景波   

  1. 陕西师范大学旅游与环境学院
  • 收稿日期:2014-05-21 修回日期:2014-09-28 出版日期:2015-01-25 发布日期:2015-04-15
  • 通讯作者: 赵景波 陕西师范大学旅游与环境学院 E-mail:zhaojb@snnu.edu.cn
  • 作者简介:李如意(1990—),女,陕西西安人,硕士生,主要从事环境评价与治理方面的研究。E-mail:lry6636@163.com
  • 基金资助:

    国家社会科学基金重大项目(11&ZD097); 中国博士后科学基金(2013M532014)

Extreme Temperature Change of Shangzhou in Recent 60 Years

LI  Ru-Yi, ZHAO  Jing-Bo   

  1. College of Tourism and Environment,Shaanxi Normal University
  • Received:2014-05-21 Revised:2014-09-28 Online:2015-01-25 Published:2015-04-15
  • Contact: ZHAO Jing-Bo College of Tourism and Environment,Shaanxi Normal University E-mail:zhaojb@snnu.edu.cn

摘要: 研究带有地理界线性质区域的山地气候有益于揭示气候变化中全局与局部关系及气候变化的复杂机理。根据1955—2012 年日气温资料,综合运用线性趋势分析、累计距平分析、Morlet 复数小波分析、滑动T 检验法、Mann-Kendall 法和主成分分析等方法,选取国际通用的表征极端气温的9 项指数,对秦岭腹地商州地区的极端气温变化进行分析,结果表明:(1)商州近60 a 平均气温呈缓慢上升趋势,四季变化趋于缓和。(2)极端最低气温、极端最高气温、气温年较差、冷夜日数和暖日日数分别以不同速率上升,高温日数、霜冻日数、暖夜日数和冷日日数分别以不同速率下降。(3)商州极端最低、最高气温以及白天、夜晚气温变化具有明显的非对称性。(4)极端气温指数存在16、22 和30 a 左右的变化周期,30 a 左右为第1 主周期。(5)9 个极端气温指数均发生突变,突变年份集中在1990—2001 年。(6)极端高温和昼指数的变化最明显,各冷指数之间以及各暖指数之间相关关系显著。最后,对商州的自然灾害及预防提出简要意见。

关键词: 商州, 气温变化, 小波周期分析, 突变分析, 主成分分析

Abstract: The research on mountain climate of a natural area with a geographic boundary is beneficial to reveal the complex mechanism governing the relation between local and global climate change. Based on the daily temperature data from 1955 to 2012, with 9 international commonly used index ,and the methods of linear trend analysis, accumulative anomaly, Morlet complex wavelet, moving T- test, Mann-Kendall examinationand principal component analysis are comprehensively employed to analyze the temporal variability of climate extremes of Shangzhou hinterland of Qinling region.The study found that:(1)The average temperature slowly increasedand the changesbetweenseasons lessenedin the past 60 years in Shangzhou .  (2)The extreme minimum temperature, extreme maximum temperature, annual temperature range, cold nights, warm days increased at different rate, while high temperature, frost days, warm nights, cold days decreased at different rates. (3)It is a clear asymmetric change of air temperature between the highest and lowest temperature and the relationship of temperaturechanges bwtween daytime and night. (4) All the extreme temperature indices have cycles of 16 , 22  and 30 years, with 30 years to be the dominating cycle. (5)Nine extreme temperature indices experienced mutation, and the mutation year concentrated in 1990s. (6)Changes in extreme high temperature and diurnal index are the most obvious, and the correlation between the cold index and the warm index is remarkable. On the bases of the research data and conclusions, comments have been made to the prevention of natural disasterin Shangzhou area.

Key words: Shangzhou, extreme temperature, wavelet analysis, mutation analysis, principal component analysis

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