长江科学院院报 ›› 2017, Vol. 34 ›› Issue (10): 17-23.DOI: 10.11988/ckyyb.20160665

• 水资源与环境 • 上一篇    下一篇

1964—2013年汉江生态经济带干湿气候时空变化分析

张逸飞1,张中旺1,2,孙小舟1,3,龚佑海1,张志洁1,孙雨露1   

  1. 1.湖北文理学院 管理学院,湖北 襄阳 441053;
    2.中国地质大学武汉 地球科学学院, 武汉 430074;
    3.中国科学院 地理科学与资源研究所,北京 100101
  • 收稿日期:2016-06-29 修回日期:2016-08-04 出版日期:2017-10-01 发布日期:2017-10-25
  • 通讯作者: 张中旺(1966-),男,湖北孝感人,教授,硕士生导师,博士,主要从事区域资源环境保护及可持续发展方面的研究,(电话)15971082393 (电子信箱) zhangzwxf@163.com。
  • 作者简介:张逸飞(1992-),男,湖北襄阳人,硕士研究生,研究方向为区域资源开发与环境保护,(电话)18850142798(电子信箱)zhangyifei0304@126.com。
  • 基金资助:
    湖北省教育厅人文社科重点项目(16D090)

Spatiotemporal Changes of Dry-wet Climatic in HanjiangRiver Ecological Economic Region During 1964-2013

ZHANG Yi-fei1, ZHANG Zhong-wang1,2, SUN Xiao-zhou1,3, GONG You-hai1,ZHANG Zhi-jie1, SUN Yu-lu1   

  1. 1.School of Management, Hubei University of Arts and Science, Xiangyang 441053, China;
    2.School of Earth Science, China University of Geosciences, Wuhan 430074, China;
    3.Institute of Geographical Science and Resources, Chinese Academy of Sciences, Beijing 100101, China
  • Received:2016-06-29 Revised:2016-08-04 Published:2017-10-01 Online:2017-10-25

摘要: 根据1964—2013年汉江生态经济带气象站点的逐日观测数据,通过气候斜向率、Kriging插值法、M-K突变检验、小波分析等手段分别对各干湿要素进行趋势、空间、突变、周期分析。结果显示:该区域总体上经历了由湿变干的过程,年降水量、潜在蒸散量、干湿指数、水分盈亏量均呈线性下降趋势,突变分别发生于2005,1972,2006,2005年前后,且存在5,15,25 a左右时间尺度的干湿周期;该区域分为湿润、半湿润地区,各干湿气候要素在空间上基本呈 “山区少、平原多”沿汉江自东南向西北逐渐变干的格局。综上,受多因素的影响,汉江中下游流域干湿气候空间分布相对复杂并逐渐变干,这种趋势已经凸显,应予以必要的重视,并采取科学可行的防旱减灾措施应对干湿气候变化。

关键词: 汉江生态经济带, 干湿气候, 时空变化, 年际变化, 突变, 防旱减灾

Abstract: According to the daily observation data of meteorological stations in the Hanjiang river ecological economic region from 1964 to 2013, we analyzed the trends, spatial changes, abrupt changes and cycles of dry-wet climate factors through climate inclination rate, Kriging interpolation, M-K mutation test, and wavelet analysis. Results suggest that the study region generally experienced a change from wet to dry. Annual precipitation, potential evapotranspiration, dry-wet index and water deficit all displayed a linear downward trend, with their sudden changes happened in 2005, 1972, 2006, and 2005, respectively. The dry-wet cycle is 5-year, 15-year and 25-year in time scale. Moreover, the study region can be roughly divided into humid and semi-humid regions, and each dry-wet climate factor presents a trend of “small in mountainous area and large in plain area” in space, which gradually becomes dry along the Hanjiang river from the southeast to the northwest. In conclusion, the dry-wet climate in the Hanjiang river basin is relatively complex and has gradually become dry. We should pay necessary attention to it and take scientific and feasible drought-resisting measures in response to dry-wet climate change.

Key words: Hanjiang river ecological economic region, wet-dry climate, spatio-temporal changes, interannual variation, abrupt change, drought relief and disaster reduction

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