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大兴安岭北坡参考植物蒸发蒸腾的经验公式

邴龙飞1,2;李秀珍1;胡远满1;王宪伟1,2;吕久俊1,2   

  1. 1中国科学院沈阳应用生态研究所, 沈阳 110016; 2中国科学院研究生院, 北京 100039
  • 收稿日期:2008-04-23 修回日期:1900-01-01 出版日期:2009-01-10 发布日期:2009-01-10

An experiential formula about the evapotranspiration of reference vegetation on northern slope of Great Hing’an Mountains.

BING Long-fei1,2;LI Xiu-zhen1;HU Yuan-man1;WANG Xian-wei1,2;LÜ Jiu-jun1,2   

  1. 1Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China;2Graduate University of Chinese Academy of Sciences, Beijing 100039, China
  • Received:2008-04-23 Revised:1900-01-01 Online:2009-01-10 Published:2009-01-10

摘要: 使用时间序列分析对大兴安岭北坡大片连续多年冻土区小流域参考植物的蒸发蒸腾进行了探讨。从年内变化规律来看,参考植物的蒸发蒸腾(ET0)呈现明显的周期性波动。蒸发蒸腾从年初开始不断增加,至7月前后达到最大值,之后逐渐减少,到年末降至最低。ET0与太阳净辐射(Rn)、白昼长度(N)分别具有明显的相关关系,利用2年气象数据建立了阿木尔流域ET0与太阳净辐射、白昼长度之间的线性关系式:ET0=0.260Rn-0.036N+0.422,可为进一步研究冻土植被的生态水文过程提供参考。

关键词: ComGIS, 景观格局, 景观监测, 管理信息系统

Abstract: By the method of time series analysis, the evapotranspiration of reference vegetation in the small watersheds of continuous permafrost on the northern slope of Great Hing’an Mountains was approached. The results showed that the evapotranspiration of the reference vegetation, ET0, had an obvious periodic fluctuation within a year, i.e., from relatively low at the beginning of the year to high before or after July, and declining to the lowest by the end of the year. The ET0 had significant correlations with net radiation (Rn) and daylight hours (N), and the formula ET0=0.260Rn-0.036N+0.422 was established, based on the two years meteorological data of Amur basin, which would benefit to the further studies on the eco-hydrological processes in the permafrost areas of northern Great Hing’an Mountains.

Key words: ComGIS, Landscape pattern, Landscape monitoring, Management information system