地理研究 ›› 2019, Vol. 38 ›› Issue (7): 1820-1832.doi: 10.11821/dlyj020190088
收稿日期:
2019-01-28
修回日期:
2019-06-02
出版日期:
2019-07-20
发布日期:
2019-07-12
作者简介:
作者简介:孙艺杰(1991-),女,辽宁兴城人,博士研究生,主要研究方向为资源环境与GIS。E-mail:
基金资助:
Yijie SUN(), Xianfeng LIU(
), Zhiyuan REN, Shuangshuang LI
Received:
2019-01-28
Revised:
2019-06-02
Online:
2019-07-20
Published:
2019-07-12
摘要:
明晰黄土高原干旱特征对于生态工程建设和社会经济可持续发展具有至关重要的作用。基于1960—2016年黄土高原59个气象台站数据和标准化降水蒸散指标(SPEI),本文分析了黄土高原多尺度干旱时空变化特征,并探讨了遥相关指数对黄土高原干旱变化的影响。结果表明:① 黄土高原SPEI指数呈下降趋势,其中70年代初和90年代末为显著干旱时期,80—90年代初为较湿润时期;② 年尺度SPEI呈下降趋势的区域遍布整个黄土高原,以山西西部、宁夏北部和甘肃中东部最为显著,而黄土高原西北和西南部则表现为变湿趋势;③ 春、夏和秋三季SPEI均呈下降趋势,且夏、秋季下降趋势较大,趋势系数均为-0.03/10a。春季干旱趋势与年际变化较为一致,秋季干旱趋势范围较大,占总面积的64.53%,冬季干旱范围较小且不显著;④ 多尺度干旱同时受IOD、NAO、PDO、AMO和ENSO3.4等遥相关指数的共同影响,且该影响存在明显的年际和年代际相位转换特征。多元回归分析显示,IOD和NAO对黄土高原干旱解释率较高,分别为22.98%和12.23%,而ENSO3.4解释率较低,表明黄土高原降水变化与西南季风具有较好的关联性。
孙艺杰, 刘宪锋, 任志远, 李双双. 1960—2016年黄土高原多尺度干旱特征及影响因素[J]. 地理研究, 2019, 38(7): 1820-1832.
Yijie SUN, Xianfeng LIU, Zhiyuan REN, Shuangshuang LI. Spatiotemporal variations of multi-scale drought and its influencing factors across the Loess Plateau from 1960 to 2016[J]. GEOGRAPHICAL RESEARCH, 2019, 38(7): 1820-1832.
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