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昆明城市热岛效应变化特征研究

孙绩华 冯健武 段玮

孙绩华, 冯健武, 段玮. 昆明城市热岛效应变化特征研究[J]. 气候与环境研究, 2015, 20(6): 645-653. doi: 10.3878/j.issn.1006-9585.2015.15072
引用本文: 孙绩华, 冯健武, 段玮. 昆明城市热岛效应变化特征研究[J]. 气候与环境研究, 2015, 20(6): 645-653. doi: 10.3878/j.issn.1006-9585.2015.15072
SUN Jihua, FENG Jianwu, DUAN Wei. Change in the Urban Heat Island Effect in Kunming[J]. Climatic and Environmental Research, 2015, 20(6): 645-653. doi: 10.3878/j.issn.1006-9585.2015.15072
Citation: SUN Jihua, FENG Jianwu, DUAN Wei. Change in the Urban Heat Island Effect in Kunming[J]. Climatic and Environmental Research, 2015, 20(6): 645-653. doi: 10.3878/j.issn.1006-9585.2015.15072

昆明城市热岛效应变化特征研究

doi: 10.3878/j.issn.1006-9585.2015.15072
基金项目: 国家自然科学基金项目41030106、41165001、41205067。

Change in the Urban Heat Island Effect in Kunming

  • 摘要: 利用昆明周边多个自动气象站观测的2004~2012年温度序列,研究了昆明城市热岛效应的日、季节 和年际变化特征,并分析了昆明城市热岛水平分布和变化趋势。昆明城市热岛强度具有明显的日变化,夜间较 强,白天较弱。城市热岛强度一般在早上08:00(北京时间,下同)达到最大值,在午后14:00减弱或消失。城市热岛强度在冬季最强,春、秋季次之,夏季最弱。昆明城市热岛强度多年平均值为1.27 ℃,在2004~2009年期间表现为逐年递减的趋势,其年际变化的主要影响因子是云量。2004~2007年昆明城市热岛中心主要分布在主 城区。2008年以后,由于中小城镇经济和人口的迅速发展,昆明城市热岛面积不断扩大,并出现热岛中心向呈 贡、石林一带偏移的现象。
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出版历程
  • 收稿日期:  2015-03-28
  • 修回日期:  2015-05-21

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