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JOURNAL OF DESERT RESEARCH  2013, Vol. 33 Issue (5): 1501-1510    DOI: 10.7522/j.issn.1000-694X.2013.00216
Weather and Climate     
Spatial Difference of Microclimate in the Oasis-Desert Ecotone in Cele, Xinjiang, China
MAO Dong-lei1,2,3,4, LEI Jia-qiang1,3, LI Sheng-yu1, REHEMUTUL Zainula1,3,4,5, WANG Cui1,3,4, ZHOU Jie1,3,4
1.Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
2.The Geographical and Tourism College of Xinjiang Normal University, Urumqi 830054, China;
3.Cele National Station of Observation and Research for Desert-Grassland Ecosystem in Xinjiang, Cele 848300, Xinjiang, China;
4.University of Chinese Academy of Sciences, Beijing 100049, China;
5.Science Branch, Xinjiang Education Institute, Urumqi 830043, China
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Abstract  

Analysis was done to the differences in time and space of monthly wind velocity, temperature, relative humidity and photosynthetically active radiation in four different underlying surfaces between ecotone and oasis in 2011. Additionally, a fine day in summer were chosen to synchronously analyze meteorological factors by comparing with sand-storm day, floating dust day, blown sand day and wet day. The results showed that: the monthly wind velocity in semi-fixed sandy land, fixed sandy land and oasis at the height of 2 m was 25.22%, 27.93% and 65.27% less, respectively, than that in mobile sandy land in June; the monthly temperature at the height of 0.5 m in oasis was higher than the rest three sites by 1.39 ℃, 1.21 ℃ and 2.70 ℃, respectively; the difference of temperature and relative humidity between May and October between the four underlying surfaces was greater than that of winter and spring; in July, the monthly temperature at the height of 2 m in mobile sandy land was higher than semi-fixed sandy land, fixed sandy land, oasis by 0.35 ℃, 1.61 ℃, 3.75 ℃, respectively; the wind velocity in sand-dust storm day was less than blown sand day, floating dust weather and wet day in turn; the air temperature in blown dust weather and fine day decreased gradually from mobile sandy land to oasis; while the relative humidity increased gradually and the difference between the four sites; the difference of air temperature and relative humidity at the four sites in sand storm weather and wet and cheerless weather was not obvious; difference of air temperature and relative humidity between blown sand day was more than that in wet day and less than that in blown dust day and fine day; difference of photosynthetically active radiation between the four sites was most obvious in day with sand-dust storm, there was no obvious difference between the day with blown dust and wet day.

Key words:  Cele      oasis-desert ecotone      oasis      microclimate      spatial difference     
Received:  30 April 2012      Published:  29 August 2012
ZTFLH:  P463.2  

Cite this article: 

MAO Dong-lei1,2,3,4, LEI Jia-qiang1,3, LI Sheng-yu1, REHEMUTUL Zainula1,3,4,5, WANG Cui1,3,4, ZHOU Jie1,3,4. Spatial Difference of Microclimate in the Oasis-Desert Ecotone in Cele, Xinjiang, China. JOURNAL OF DESERT RESEARCH, 2013, 33(5): 1501-1510.

URL: 

http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2013.00216     OR     http://www.desert.ac.cn/EN/Y2013/V33/I5/1501

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