植物生态学报 ›› 1989, Vol. 13 ›› Issue (3): 197-207.

• 论文 •    下一篇

植被的PE(可能蒸散)指标与植被-气候分类(二)——几种主要方法与PEP程序介绍

张新时   

  • 发布日期:1989-03-10
  • 通讯作者: 张新时

The Potential Evapotranspiration (PE) Index for Vegetation and Vegetation-Climatic Classification (2) -an Introduction of Main Methods and PEP Program

Chang Hsin-shih   

  • Published:1989-03-10
  • Contact: Wu Zeng-zhi

摘要: 应用C.W.Thorn thwaite计算PE与气候分类方法对我国671个气候台站资料计算分析结果,得出可能蒸散的地理回归模型为:APE=2037.98-18.8308LAT(纬度)-4.5801LONG(经度)-0.157861ALT(海拔)APE与湿度指数Im与我国植被的主要类型及其分布格局有密切相关性。其热量指标(APE)界限与北美颇相符合,但Im明显偏低,反映了中国植被的生态特点。研究表明该方法在我国有明显的应用前景。

Abstract: Thornthwaite’s method on calculating PE and climatic classification has been applied on computing data from 671 climatological observation stations in China. A geographic regression model of potential evapotran-spiration is resulted as APE=2037.98—18.8308 LAT—4.5801 LONG—0.157861ALT. The resulted APE and moisture index, Im are closely correlated with the major vegetation types and their distribution pattern in China. The bounds of thermal coefficient (APE) for the vegetation in China fits in quite well with which in North America, but the Im is evidently lower than there. That just is a reflection of the ecological characteristics for vegetation of China. The research makes known that the method should have a broad prospect for application in the country.