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中国沙漠 ›› 1999, Vol. 19 ›› Issue (2): 97-103.

• 论文 •    下一篇

新疆伊犁地区现代气候特征与300 a来的干湿变化规律

叶玮1, 袁玉江2   

  1. 1. 中国科学院新疆生态与地理研究所, 乌鲁木齐 830011;
    2. 新疆气象局气象科研所, 乌鲁木齐 830002
  • 收稿日期:1998-11-30 修回日期:1998-12-15 出版日期:1999-06-20 发布日期:1999-06-20
  • 作者简介:叶玮(1957-),女,博士,副研究员。主要从事干旱区地貌与第四纪环境方面的研究工作。
  • 基金资助:
    国家自然科学基金项目(49671009)资助

The Modern Climatic Characteristics and Dry Wet Fluctuations in the Past 300 Y ears in Yili Area, Xinjiang

YE Wei1, YUAN Yu-jiang2   

  1. 1. Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
    2. Xinjiang Institute of Meteorology, Urumqi 830002, China
  • Received:1998-11-30 Revised:1998-12-15 Online:1999-06-20 Published:1999-06-20

摘要: 在现代实测资料分析和利用树木年轮对伊犁地区314a降水重建研究的基础上,通过与历史资料在时间上的对比以及与中亚、中国东部和北疆地区小冰期以来气候变化模式在空间上的对比分析,发现300a来伊犁地区的气候变化不仅具有冷与湿、暖与干相对应的特点,而且偏干年出现的频率多于偏湿年。在气候的干湿波动中,湿润期变短,而干旱期相对增长,反映了该区300a来气候与北疆其它地区类似,在波动中存在着变干的趋势。

关键词: 伊犁地区, 气候特征, 干-湿变化

Abstract: This paper has analyzed the characteristics of the climatic changes based on the current meteorology data in the recent 40 years of 9 meteorological stations in Yili area. Through 5 tree ring chronology series, the 314 year precipitation was well reconstructed and its explain variance was 75%. The paper also has com pared th e features of climatic changes in Yili with the neighboring areas(the other area s of Xinjiang, Gansu, Qinhai provinces, China and Central Asia), and obtained some beneficial results as follows: (1) Maximum entropy spectrum analysis showed that annual temperature change had 2, 4.25 and 10~11 years significant periodicity in recent 35 years. The re was an evident warming tendency from 1953 to 1995, and the rising rate of mean annual temperature was 0.28℃/10a. Contrast to the annual temperature, the magnitude of winter temperature increase was larger in recent 25 years. Th e rising rate reached 1.6℃/10a that is as 4.7 times as that of th e annual. The change is consistent with those of other areas of China and Northern Hemisphere in rec ent decades. That is the temperature of Yili area responded to the global change better. (2) The precipitation of annual and seasons in Yili area has better correlation to that in the other areas of Northern Xinjiang and Central Asia, but is not related to that in the other areas of Northwest China, Qinzhang Plateau and East China. This suggests that the difference of precipitation between monsoon and westerly belt is bigger than that of temperature. (3) In the past 314 years, the series of reconstructed precipitation had 4 w et periods above its mean and 4 dry periods bellow the mean. The wet periods were getting short and dry ones changed conversely. It is obvious that the climate changes toward warm and dry, which is related to the global change since beginning of this century. (4) The climatic patterns that cold match wet and warm match dry are predominant in the past 314 years, which is similar to the change of modern climate.

Key words: Yili region, Climatic characteristics, Dry-wet fluctuation

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