北京大学学报(自然科学版)

NDVI与气候因子耦合关系及其地域差异的定量递归分析
--以云南省纵向岭谷区为例

李双成1, 刘逢媛1, 戴尔阜2, 吴绍洪2   

  1. 1北京大学城市与环境学院,地表过程分析与模拟教育部重点实验室,北京 100871; 2中国科学院地理科学与资源研究所,北京 100101;
  • 收稿日期:2007-05-09 出版日期:2008-05-20 发布日期:2008-05-20

Recurrence Quantification Analysis for Geographical Differences of the Coupling Relationship between NDVI and Climatic Factors

LI Shuangcheng, LIU Fengyuan1, DAI Erfu2, WU Shaohong2   

  1. 1College of Urban and Environmental Sciences, Peking University, Laboratory for Earth Surface Processes, Beijing 100871;2Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101;
  • Received:2007-05-09 Online:2008-05-20 Published:2008-05-20

摘要: 以云南省纵向岭谷区南部西南季风区和东南季风区为例,采用定量递归(recurrence quantification analysis,RQA)和交叉递归图(cross recurrence plots, CRP)方法分析了NDVI和气候因子之间的相互关系。结果表明,云南省纵向岭谷区西南季风区NDVI系列的确定性高于其东南季风区,两区NDVI系列耦合关系的动力学特性介于完全随机系列与含有噪声的确定性系列之间。从整体上看,两区NDVI系列的同步性较差,特别是在1987?1989年和1991?1993年两个时段同步性最低,而且西南季风区NDVI系列的变化滞后于东南季风区。从两个季风区NDVI分别与降水、气温系列耦合关系的CRP指数看,西南季风区NDVI与降水关系的相似性及其延存时间、结构性以及稳定程度均高于东南季风区, NDVI与气温关系与上述趋势大体一致,但各CRP指数在两个气候区的差别更小,说明NDVI与气温相互作用的特征在两区差异较小。

关键词: 交叉递归图, NDVI, 气候因子, 云南省纵向岭谷区

Abstract: Recurrence quantification analysis (RQA) and cross recurrence plot (CRP) are used to analyze the relationship between the normalized difference vegetation index (NDVI) and climatic factors in the Southwest and Southeast Monsoon Regions in Yunnan longitudinal range-gorge region (LRGR). Results show that in the Southwest Monsoon Region the NDVI series has a higher certainty than that in the Southeast Monsoon Region. The coupling relationships of NDVI series in the two regions are between a completely random series and a deterministic series with noise. The two NDVI series have low synchronization in general, especially in the period 1987?1989 and 1991?1993. The NDVI series of the Southwest Monsoon Region lags behind that of the Southeast Monsoon Region. According to the CRP indices, the similarity, persistence time and stability of the coupling relationship between NDVI and precipitation series in the Southwest Monsoon Region are better than that of the Southeast Monsoon Region. Both the NDVI series and temperature series have similar trends. However, the difference of the CRP indices between the two regions is smaller. It is suggested that the interaction pattern of NDVI and temperatures has a smaller difference between the two regions.

Key words: cross recurrence plots, NDVI, climatic factors, Yunnan LRGR

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