南京大学学报(自然科学版) ›› 2015, Vol. 51 ›› Issue (3): 543–.

• • 上一篇    下一篇

长三角地区人为热时空分布特征研究

朱宽广1,谢 旻1*,王体健1,杨浩明2,廖镜彪1   

  • 出版日期:2015-04-23 发布日期:2015-04-23
  • 作者简介:(1.南京大学大气科学学院,南京,210093;2.南京信息工程大学大气物理学院,南京,210044)
  • 基金资助:
    国家重点基础研究发展规划(973)项目(2010CB950704,2010CB428503),江苏省基础研究计划(自然科学基金)资助项目(BK2011578),国家自然科学基金项目(40805059)资助项目

Study of the temporal and spatial variation of anthropogenic heat flux over YRD
Zhu Kuanguang1, Xie Min1*, Wang Tijian1, Yang Haoming2,Liao Jingbiao1

Zhu Kuanguang1, Xie Min1*, Wang Tijian1, Yang Haoming2,Liao Jingbiao1
  

  • Online:2015-04-23 Published:2015-04-23
  • About author:(1. School of Atmospheric Science, Nanjing University, Nanjing, 210093, China;
    2. School of Atmospheric Physics, Nanjing University of Information Science and Technology, Nanjing,210044, China)

摘要: 根据中国统计年鉴中各地区能源消费资料和人口数据,研究了长三角城市群的人为热排放,对其进行了时间和空间上的分析,讨论了长三角地区的人为热分布特点及影响因素。结果表明,长三角地区的人为热释放量是随时间持续增长的,上海地区的年均人为热通量从1990年的5.47W/m2到2010年增加为14.46 W/m2,江苏和浙江也分别从0.68、0.33 W/m2增加到2.61、1.63W/m2;人为热释放空间分布不均匀,总体上来说还是以城区为高值中心,向郊区逐渐减小,这种分布与人口密度、工业和经济发展程度密切相关。此外,长三角整个区域的人为热通量都高出全国平均值一个量级以上,而且高值区域已经初步连成一片,人为热将对区域气候造成一定影响。从1990年到2000年,长三角16个城市的城区的人为热通量都是稳步增长的;2000年后人为热通量开始快速增长,增长速度最高可达2W/m2/yr。城市人为热排放愈来愈强,对城市局地小气候和空气污染影响将越来越重要。

Abstract: Based on the energy consumption data and demographic data of Yangtze River Delta region (YRD), the temporal and spatial variation of anthropogenic heat flux (AHF) in YRD was estimated. The characteristics and the influence factors were discussed. The results show that AHF over YRD has been growing from 1990 to 2010. The annual mean values of Shanghai, Jiangsu and Zhejiang have increased from 5.47, 0.68, 0.33 W/m2 to 14.46, 2.61, 1.63 W/m2 respectively in two decades. The spatial distribution of AHF, which is related to the population density, the industrial level and economic development, is uneven. The value in YRD is one order of magnitude larger than that for the national average. The value in the urban center is higher than that in the surrounding areas. From 1990 to 2000, the AHF of the 16 core cities in YRD grew steadily. However, the growth accelerated after 2000, and the maximum rate can get to 2 W/m2 a year. The stronger the AHF is, the more important the effects of AHF on local microclimate and air pollution will be

[1]. Chaisson E J. Long-term global heating from energy use. Eos Trans AGU, 2008, 89(28): 253, doi:10.1029/2008EO280001.
[2]. Ichinose T K Shimodozono, Hanaki K. Impact of anthropogenic heat on urban climate in Tokyo. Atmos Environ, 1999, 33: 3897-3909.
[3]. Khan S M, Simpson R W.Effect of a heat island on the meteorology of a complex urban airshed.Boundary-Layer Meteorology,2001, 100: 487-506.
[4]. Block A, Keuler K, Schaller E. Impacts of anthropogenic heat on regional climate patterns.Geophysical Research Letters, 2004, 31(12): ~ .
[5]. Narumi D, Shimoda Y, Kondo A, et al.Effect of anthropogenic waste heat upon urban thermal environment using mesoscale meteorological model.Fifth International Conference on Urban Climate, Lodz, Poland, 2003.
[6]. Hamilton I G, Davies M, Steadman P, et al. The significance of the anthropogenic heat emissions of London’s building: A comparison against captured shortwave solar radiation. Building Environ,2009, 44, 807-817
[7]. Makar P A, Gravel S, Chirkov V, et al. Heat flux, urban properties, and regional weather. Atmos Environ,2006, 40, 2750-2766
[8]. Mark G Flanner. Integrating anthropogenic heat flux with global climate models. Geophysical Research Letters,2009, 36: L02801, doi:10.1029/2008GL036465,2009
[9]. 陈 兵,石广玉,戴 铁等. 中国区域人为热释放的气候强迫. 气候与环境研究,2011, 16 (6): 717-722.
[10]. Ichinose T K Shimodozono, Hanaki K. Impact of anthropogenic heat on urban climate in Tokyo. Atmos Environ, 1999, 33: 3897-3909.
[11]. Sailor D J, Lu L. A top-down methodology for developing diurnal and seasonal anthropogenic heating profiles for urban areas. Atmos Environ,2004, 38: 2737-2748
[12]. Fan H, Sailor D J. Modeling the impacts of anthropogenic heating on the urban climate of Philadephia: A comparision of implementations in two PBL schemes. Atmos Environ, 2005, 39: 73-84.
[13]. Lee S H, Song C L, Baik J J, et al. Estimation of anthropogenic heat emission in the Gyeong-In region of Korea. Theor Appl Climatol,2009, 96:291-303.
[14]. Quah A K L, Roth M. Diurnal and weekly variation of anthropogenic heat emissions in a tropical city, Singapore.Atmospheric Environment, 2012, 46: 92-103.
[15]. 佟 华,刘志辉,桑建国等. 城市人为热对北京热环境的影响, 气候与环境研究,2004, 9 (3): 409-421.
[16]. 何晓凤,蒋维楣,陈 燕等. 人为热源对城市边界层结构影响的数值模拟研究. 地球物理学报,2007,50(1):74-82.
[17]. 陈 曦,王咏薇. 2011.2001年至2009年中国分省人为热通量的计算和分析[C]. 第28届中国气象学会年会——S7城市气象精细预报与服务,2011.
[18]. 陆 燕,王勤耕,翟一然等. 长江三角洲城市群人为热排放特征研究. 中国环境科学,2014, 34(2):295-301.
[19]. Fanger P O. Thermal comfort: Analysis and Applications in Environmental Engineering. New York: McGraw-Hill, 1972, 1-244.
[20]. Fulton P N. Estimating the daytime population with the urban transportation planning package. Washington D C: Transportation Research Record, 1984: 25-27.
No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!