THE TIME-SPACE CHANGE OF PRECIPITATIONAND ARIDITY DEGREE OF SONGNEN SANDLAND SINCE LAST GLACIAL AGE

Expand
  • Department of Geography, Northeast Normal University, Changchun 130024

Received date: 1994-09-07

  Revised date: 1995-01-15

  Online published: 1995-07-20

Abstract

Songnen sandland lying in the middle of northeast China is in the continental monsoon climatic region of transitional belt between semi-humid and semi-arid temperate zone. It is the first-grade susceptible belt of environmental evolution in China.Since the last glacial age, the nature environment of Songnen sandland have undergone complex evolution process. Based on the principle that vegetation is related to precipitation and aridity degree, using pluralistic linear regression analysis, the authors calculated quantitatively the precipitetion and aridity degree of Songnen sandland since the last glacial age, and drew the change curves of precipitation and aridity degree in different periods, and 1.1-1.2 isogram of aridity degree. Since the last glacial age Songnen sandland underwent 5 periods of high precipitation and low aridity degree. And the east boundary of the sandland in different periods have also been estimeted.

Cite this article

Jie Dongmei, Lu Jinfu . THE TIME-SPACE CHANGE OF PRECIPITATIONAND ARIDITY DEGREE OF SONGNEN SANDLAND SINCE LAST GLACIAL AGE[J]. SCIENTIA GEOGRAPHICA SINICA, 1995 , 15(4) : 337 -343,393 . DOI: 10.13249/j.cnki.sgs.1995.04.337

References

[1] 史培军.地理环境演变研究的理论与实践.北京:科学出版社,1992. 79-81.
[2] Swain A M et al. Estimate of Holocene precipitation for Rajasthan India,based on pollen and lakc-Icvcl data.Quatcrnary Research, 1983. 19(1):33-43.
[3] 东北平原第四纪自然环境形成与演化课题组.中国东北平原第四纪自然环境形成与演化.哈尔滨:哈尔滨地图出版社,1991. 51-67.
[4] 施雅风,崔之久,李吉均,等.中国东部第四纪冰川与环境问题.北京:科学出版社,1989. 363-374.
Outlines

/