西宁城市热岛效应分析
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

X16

基金项目:

国家重点研发计划资助项目(2016YFC0501903)


Analysis of urban heat island effect in Xining
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    西宁作为青藏高原最大的城市,近年来随着城市化的发展,城市热岛效应及其所带来的影响日益明显。本文利用西宁市城市和郊区气象观测站逐小时气温观测资料,分析了西宁市平均气温、最高气温和最低气温日内、候平均热岛强度变化特征,结果显示:(1)相对于郊区,西宁城区平均气温日内变化幅度较小,16-17时(北京时,下同)表现为弱的冷岛效应,冷岛强度为0.034℃,日出前的06-07时热岛强度表现最强,热岛强度最高可达3.01℃;(2)春季和夏季一天中均为热岛效应,且热岛效应日内变化幅度较小,分别为2.76℃和2.12℃。秋季和冬季在日出前的07-08时热岛强度最强,分别为2.89℃和4.14℃,秋季16-17时和冬季15-17时表现为冷岛效应,最大冷岛强度分别为0.34℃和0.53℃;(3)西宁城区1月第3候热岛强度最强为3.40℃,7月第2候热岛强度最弱为1.07℃。其中白天在1月第3候热岛强度最强为0.88℃,9月第1候最弱为0.13℃,热岛强度年内变幅较小仅为0.75℃,而夜晚在1月第3候最强为5.93℃,7月第2候最弱为1.62℃,热岛强度年内变化幅度达4.30℃;(4)西宁城区候平均最高气温在春季和夏季表现为热岛效应,热岛强度平均为0.58℃,而在秋冬季表现为冷岛效应,冷岛强度分别为1.84℃。候平均最低气温全年均表现为热岛效应,其中夏季相对较弱为3.22℃,冬季表现最强达到5.11℃。

    Abstract:

    With the development of urbanization, Xining, the largest city on the Qinghai-Tibet Plateau, its urban heat island effect and impact are increasingly obvious in recent years. Based on hourly temperature data from meteorological observation stations in Xining city and suburbs, this paper analyzed the variation characteristics of daily and hourly average heat island intensity of average temperature, maximum temperature and minimum temperature in Xining city. The results show:(1) Compared with the suburbs, the average temperature in Xining city had a small change within a day, showing a weak cold island effect from 16:00 to 17:00. The intensity of cold island was 0.034℃, and the intensity of heat island was strongest from 06:00 to 07:00 before sunrise, with the highest intensity of heat island reaching 3.01℃; (2) Both spring and summer were heat island effects in one day, and the change range of heat island effect in one day is small, 2.76℃ and 2.12℃, respectively. The intensity of heat island was strongest in autumn and winter at 07:00-08:00 before sunrise, which are 2.89℃ and 4.14℃, respectively. The cold island effect was shown in autumn at 16:00-17:00 and winter at 15:00-17:00, and the maximum cold island intensity is 0.34℃ and 0.53℃, respectively. (3) The strongest mean temperature UHI intensity was 3.40℃ at the third five-day in January, and the weakest UHI intensity was 1.07℃ at the second five-day in July. The UHI intensity showing obvious at the third five-day in January was 0.88℃, and it showing weakest at the first five-day in September was 0.13℃ in the day. But in the night, the maximum UHI intensity was 5.92℃ at the third five-day in January, and the minimum value was 1.62℃ at the second five-day in July. So the variations range of seasonal UHI intensity in the night was obvious than in the day, and the value was 4.30℃ and 0.75℃; (4) The average extreme maximum temperature showed UHI effect in spring and summer, and the average UHI intensity was 0.58℃, but it showed urbane cold island effect in autumn and winter, and the value was 1.84℃. The average extreme minimum temperature showed UHI effect all the time, and the UHI intensity was 3.22℃and 5.11℃ in summer and winter.

    参考文献
    相似文献
    引证文献
引用本文

李红梅,樊万珍.西宁城市热岛效应分析.气象科学,2019,39(4):562-568 LI Hongmei, FAN Wanzhen. Analysis of urban heat island effect in Xining. Journal of the Meteorological Sciences,2019,39(4):562-568

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2018-02-22
  • 最后修改日期:2018-06-02
  • 录用日期:
  • 在线发布日期: 2019-08-31
  • 出版日期:
您是第位访问者
气象科学 ® 2024 版权所有
技术支持:北京勤云科技发展有限公司