本文已被：浏览 588次 下载 1194次
中文摘要: 本文根据美国著名生物气象学家R·G·Steadman提出的感热温度理论,计算了我国各地夏季(6—8月)各月平均14时感热温度,讨论了空气湿度、风速对感热温度的影响,并计算了长江流域和华南地区夏季逐日感热温度,分析比较了这两个地区夏季酷热的天气气候特征。
中文关键词:
Abstract:With a concept intiated by American bio-meteorologist R. G. Steadman, the monthly mean apparent temperatures at 14p·m. in summer (Juno to Aug.) in China are calculated, and the effects of wind and air humidity on the apparent temperature are discussed. The synoptic, and climatic features of the sweltering hot in summer in the reaches of the Changjiang River and in South China are compared by analysis of the day to day apparent temperatures in the two regions.
keywords:
文章编号： 中图分类号： 文献标志码：
基金项目:
| Author Name | Affiliation |
引用文本：
冯定原,邱新法,黄桔梅,1989.我国夏季感热温度的分布[J].气象,15(6):21-26.
,1989.The distribution of the apparent temperatures in summer in China[J].Meteor Mon,15(6):21-26.
冯定原,邱新法,黄桔梅,1989.我国夏季感热温度的分布[J].气象,15(6):21-26.
,1989.The distribution of the apparent temperatures in summer in China[J].Meteor Mon,15(6):21-26.