干旱区研究 ›› 2011, Vol. 28 ›› Issue (3): 492-498.

• 天气与气候 • 上一篇    下一篇

近50年来秦岭南北气候分异研究

宋佃星1, 延军平1, 马莉2   

  1. 1. 陕西师范大学 旅游与环境学院 , 陕西 西安 710062;
    2. 宝鸡文理学院 地理科学与环境工程系, 陕西 宝鸡 721013
  • 收稿日期:2010-04-05 修回日期:2010-05-31 出版日期:2011-06-25 发布日期:2011-09-06
  • 作者简介:宋佃星(1982-),男,山东淄博人,博士,主要从事区域可持续发展研究.E-mail:starzone@Yeah.net
  • 基金资助:

    国家自然科学基金(40871052)

Study on Climatic Differentiation in the South and North Qinling Mountains in Recent 50 Years

SONG Dian-xing1, YAN Jun-ping1, MA Li2   

  1. 1. College of Tourism and Enviroment Science, Shaanxi Normal University, Xi'an 710062, China;
    2. Department of Geographic and Environmental Sciences, Baoji College of Arts & Sciences, Baoji 721013, Shaanxi Province, China
  • Received:2010-04-05 Revised:2010-05-31 Online:2011-06-25 Published:2011-09-06

摘要: 全球变化就区域性而言,重点集中在脆弱生态区和自然地理区域的过渡地带,如海岸线、水分条件充足的堤度带及山地。秦岭南北的气候变迁是全球气候研究的重点。研究表明:近50年来,秦岭南北平均气温呈上升趋势,但在突变时间与幅度存在一定的差异。秦岭北部在1989年发生突变,升温幅度为0.03 ℃/a,夏冬两季升温幅度大;秦岭南部在1992年发生突变,升温幅度为0.01 ℃/a,同样夏冬两季升温幅度大。降水量秦岭南北呈减少趋势,北部与南部降水量减少幅度分别为1.36 mm/a和2.66 mm/a,北部夏秋季减少幅度大,南部春秋季减少幅度大。

关键词: 气候变化, 脆弱生态地理区, 气温, 降水量, 秦岭

Abstract: As for regionality, the study emphases of global climate change are always in the ecological fragile regions and the transitional zones of physical geographic areas, such as the coastlines, mountains and the gradient zones with sufficient moisture. The Study on climate change in the south and north Qinling Mountains is of important significance in studying global climate change. In this study, the values of mean annual and seasonal temperature and precipitation were calculated based on the data observed by the meteorological stations in the south and north Qinling Mountains so as to analyze the climate change trend from the aspects of temperature and precipitation anomalies, 5-year sliding tendency and long-term sliding tendency. In order to investigate the sharp climate change, the Mann-Kendall, sliding T and Yamamoto test method were plied. The results reveal that the average temperature in the south and north Qinling Mountains was in an increase trend, but there was a certain difference in the sharp change time and range: the sharp temperature increase (0.034 ℃/a) in the north Qinling Mountains occurred in 1989, especially in summer and winter, but that (0.014 ℃/a) in the south Qinling Mountains occurred in 1992, especially in summer and winter similarly. Precipitation in the south and north Qinling Mountains was decreased, it was decreased by 2.66 mm/a in the north Qinling Mountains and by 1.36 mm/a in the south Qinling Mountains, respectively, and its reduction was high in summer and autumn in the northern Qinling Mountains but in spring and autumn in the south Qinling Mountains.

Key words: climate change, ecological fragile region, temperature, precipitation, Qinling Mountains

中图分类号: 

  • P467