收藏设为首页 广告服务联系我们在线留言

干旱区地理 ›› 1988, Vol. 11 ›› Issue (3): 25-30.doi: 10.13826/j.cnki.cn65-1103/x.1988.03.006

• • 上一篇    下一篇

塔里木河中下游年表特征

李江凤, 袁玉江, 王承义   

  1. 新疆气象科研所
  • 出版日期:1988-09-25 发布日期:2025-12-25

The Feature of the Chronological Zable in the Middle and Lower Reaches of Tarim River

Li Jiangfeng, Yuan Yujiang, Wang Chenyi   

  1. The Meteorological Institute of Xinjiang
  • Published:1988-09-25 Online:2025-12-25

摘要: 通过对沙漠与山区年轮研究中的采样、年表特征及年表中的水分信息三个问题的比较分析,阐述了塔里木河中下游年表的特征等问题,得到以下三点结论:(1)沙漠与山区采点状况不同,采样方法有异,沙漠采样注重距河的远近及地势高低,而山区采样强调林带上下限等。(2)沙漠年表的敏感度大于山区,自相关与互相关小于山区,年表中的低频周期少于山区。(3)沙漠年表的水分限制因子是流量,山区是降水,沙漠年表中的流量信息多于降水,山区相反。

关键词: 塔里木河中下游, 胡杨年表, 水分信息

Abstract: the tree-ring sampling,the feature of the chronological table and the moisture information in the chronological table in desert and mountain area have been compared and analysed in this paper.Three conclusions have been obtained.
1)The sampling methods vary with the places of sampling.The stress is laid on the distance to river and the height of terrain in desert,while the upp-er and lower limit of forest belt and other factors are emphasized in mountain area.
2)The sensitivity of the chronological table in desert is larger than that in mountain area,whereas the self correlation and mutual correlation are smaller, and the low frequency period of the table is shorter than that in mountain area.
3)The moisture limit factor is the volume of flow in the table of desert, but the precipitation in mountain area.The information of flow is more than that of precipitation,though on the contrary in mountain area.