地理科学 ›› 2010, Vol. 30 ›› Issue (4): 620-623.doi: 10.13249/j.cnki.sgs.2010.04.620

• 论文 • 上一篇    下一篇

基于热力重心的广州城市热环境时空变化分析

孙芹芹1,2, 吴志峰2,3, 谭建军2   

  1. 1. 厦门大学海洋与环境学院, 福建 厦门 361005;
    2. 中国科学院广州地球化学研究所, 广东 广州 510640;
    3. 广东省生态环境与土壤研究所, 广东 广州 510650
  • 收稿日期:2009-12-28 修回日期:2010-03-11 出版日期:2010-07-20 发布日期:2010-07-20
  • 基金资助:
    国家自然科学基金项目(40571164)资助。

Spatio-temporal Changes of Urban Thermal Environment with Thermal Centroid in Guangzhou

SUN Qin-qin1,2, WU Zhi-feng2,3, TAN Jian-jun2   

  1. 1. College of Oceanography and Environmental Science, Xiamen University, Xiamen, Fujian 361005;
    2. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, Guangdong 510640;
    3. Guangdong Institute of Eco-environment and Soil Sciences, Guangzhou, Guangdong 510650
  • Received:2009-12-28 Revised:2010-03-11 Online:2010-07-20 Published:2010-07-20

摘要: 城市热环境及其变化与城市发展关系密切,热力环境的时空变化在一定程度上反映了城市发展的空间变化格局。通过构建热力重心转移距离、热力重心转移角度以及热力重心转移贡献率3个指数,计算3个不阶段广州市城市热环境的时空变化格局。结果表明,广州市1990~2005年高温地区的热力重心一直向南迁移。城市热力重心的转移路径与城市内部各地区在不同时期的发展及扩张具有一定的关系。

Abstract: The distribution and evolution of urban thermal environment are influenced by urban development. In this study, the concept of "thermal centroid" was given to describe the distribution of urban thermal environment in Guangzhou, and three indices about it were created, including thermal diversion distance, thermal diversion direction as well as thermal diversion contribution. It was showed that, the high-temperature thermal centroid transferred to the south of Guanghzou from 1990 to 2005. During 1990-2000, Panyu District made the greatest negative contribution to the transfer, but the positive contribution was made by Panyu District during 2000-2005.

中图分类号: 

  • X16