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滇中地区夏季城市热岛效应的数值模拟研究

郑亦佳 刘树华 何萍 缪育聪 王姝

北京大学学报(自然科学版)2017,Vol.53Issue(4):639-651,13.
北京大学学报(自然科学版)2017,Vol.53Issue(4):639-651,13.DOI:10.13209/j.0479-8023.2016.127

滇中地区夏季城市热岛效应的数值模拟研究

Numerical Study of Summertime Urban Heat Island in Dianzhong

郑亦佳 1刘树华 2何萍 1缪育聪 3王姝4

作者信息

  • 1. 北京大学物理学院大气与海洋科学系,北京 100871
  • 2. 浙江省气象台,杭州 310017
  • 3. 云南楚雄师范学院地理科学与旅游管理学院,楚雄 675000
  • 4. 中国气象科学研究院,北京 100081
  • 折叠

摘要

Abstract

In order to study the effect of urbanization and lakes on the urban heat island (UHI) effect of cities in Yunnan midland in summer, the weather research forecasting model (WRF) numerical model is used. The downwind urban heat island is found in these cities in the summer night. The expansion of city will expand the scope of the downwind urban heat island, but the intensity of the heat island would not be enhanced significantly. The presence of the city will change the surface roughness, resulting in the reduction of wind speed near the surface. In the daytime, lakes and the city influence surface wind speed by changing the local thermal difference. The existence of city increases the thermal difference between city and lake, which enhances both the lake-land breeze and the surface wind speed. The presence of city will reduce the supply of low-level moisture, but the impact of urban expansion on moisture is relatively small. In the early morning, the wet island exists in the city (humidity in city is slightly larger than the surrounding area), due to the convergence filled near surface. At other moments, the dry island exists in the city (humidity in city is smaller than the surrounding area), and has the downwind effect as well.

关键词

城市热岛/湖陆风/WRF模式/滇中地区

Key words

urban heat island/lake-land breeze/WRF model/Dianzhong region

分类

天文与地球科学

引用本文复制引用

郑亦佳,刘树华,何萍,缪育聪,王姝..滇中地区夏季城市热岛效应的数值模拟研究[J].北京大学学报(自然科学版),2017,53(4):639-651,13.

基金项目

国家自然科学基金(41465001)和国家电网公司科技项目资助 (41465001)

北京大学学报(自然科学版)

OA北大核心CSCDCSTPCD

0479-8023

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