中国农业气象 ›› 2013, Vol. 34 ›› Issue (01): 81-87.doi: 10.3969/j.issn.1000-6362.2013.01.012

• 论文 • 上一篇    下一篇

东北地区作物生长季干旱时空分布特征及其环流背景

马建勇,许吟隆   

  1. 1贵州省山地环境气候研究所/贵州省山地气候与资源重点实验室,贵阳 550002;2中国农业科学院农业环境与可持续发展研究所,北京 100081
  • 收稿日期:2012-05-12 出版日期:2013-02-20 发布日期:2013-04-17
  • 作者简介:马建勇(1987-),新疆阿勒泰人,助理工程师,硕士,研究方向为气候变化。Email:majianyong2005571@163.com
  • 基金资助:

    中英瑞国际合作ACCC项目(ACCC/20100515;ACCC/003);农业部948项目(2011-G9);黔科合重大专项([2011]6003号)

Temporal and Spatial Characteristics and Circulation Background of Drought in Crop Growing Season over Northeast China

MA Jian yong, XU Yin long   

  1. 1 Guizhou Institute of Mountainous Environment and Climate/Guizhou Key Laboratory of Mountainous Climata and Resources, Guiyang 550002,China;2 Institute of Environment and Sustainable Development in Agriculture, CAAS, Beijing 100081
  • Received:2012-05-12 Online:2013-02-20 Published:2013-04-17

摘要: 依据东北地区71个气象台站1961-2009年5-9月气温、降水资料,对帕默尔干旱指数(PDSI)评价实际干旱的能力进行验证,并对PDSI距平场展开经验正交函数(EOF)分析,同时利用NCEP/NCAR再分析资料对干旱年的环流背景做了初步探讨。结果表明,(1)PDSI对东北地区农作物生长季的实际干旱具有较高评估能力,但在个别年份容易高估干旱程度;(2)EOF前3个特征向量的累积方差贡献率达74.9%。其中,第1特征向量是主要的分布格局,为全区一致型,第2特征向量为南北相反型,第3特征向量为东西相反型;(3)近49a东北地区农作物生长季干旱以9a和23a的变化周期为主,未来几年内干旱趋势仍将持续增强;(4)在干旱年(PDSI≤-1),500hPa高度场上副高偏弱,东北地区处于槽后脊前,同时该地区为位势高度距平的正中心,受高压控制降水偏少。850hPa水汽通量场上,输送到东北地区的西南及东南暖气流的水汽明显较少,同时该地区不仅存在反气旋环流,而且其水汽通量散度大于0,不利于降水。

关键词: 东北地区, 农作物生长季, Palmer干旱指数, 经验正交函数, 大气环流

Abstract: Based on observed data of mean temperature and precipitation from 71 meteorological stations in Northeast China from 1961 to 2009 in crop growing season (from May to September), authors validated Palmer Drought Severity Index (PDSI) to assess the actual drought level, and analyzed its characteristic by using Empirical Orthogonal Function(EOF) method, used the NCEP/NCAR reanalysis data to discuss the circulation background in drought years. The results showed that, (1)PDSI could assess the actual drought level with high ability in crop growing season, but it was easily to exaggerate the seriousness of drought in some years; (2)The accumulative variance contribution ratio of the first three feature vectors reached to 74.9%, and the spatial types of drought in Northeast China could be divided to three patterns: uniform, south-north difference, east-west difference, corresponding with the first three feature vectors individually;(3)During 1961 to 2009,the drought variation mainly existed 9 years and 23 years periodic oscillations in crop growing season, and the drought trend in the next few years might continue to increase; (4)In drought years(PDSI≤-1), the subtropical high presented weak performance in 500hPa height field, Northeast China was the center of positive geo potential height anomaly, indicating that the region was controlled by high pressure, resulting in less rainfall. In terms of 850hPa water vapor flux field, warm wet airflows from southwest and southeast were hardly transported to the Northeast China, and the anti cyclonic circulation and positive divergence also could lead to less precipitation.

Key words: Northeast China, Crop growing season, Palmer drought severity index, EOF, Atmospheric circulation