南京夏季城市局地气温时空变化特征
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TU119.4

基金项目:

国家自然科学基金(51408303、41871189);江苏省自然科学基金(BK20161547)


Temporal and spatial variations of local temperatures in the summer of Nanjing
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    摘要:

    城市局地气候分区(Local Climate Zone,简写为LCZ)是一套用于城市气温研究的客观、标准、通用的局地热气候分类方法。基于LCZ方法对南京城市气温进行观测,分析了2016年夏季时段(7-9月)分布于南京城区至郊区的12个不同类型LCZ地块的气温时空变化特征,包括热岛日变化特征、平均热岛强度、日最高/最低温度差异、升温/冷却率差异。结果表明:各LCZ地块的热岛强度在日落后迅速增加,日落后3~5 h达到最大值,然后逐渐减小,这一现象与各LCZ地块的升温/冷却率变化特征相对应;城市化强度越高的LCZ地块热岛强度越大;午间部分地块出现城市冷岛现象;水域区(LCZ G)在白天有一定的降温效果,夜间则会产生热岛效应;各LCZ地块的夜间平均热岛强度差异明显,日最低气温差异显著高于日最高气温差异。

    Abstract:

    The Local Climate Zone (LCZ) scheme aims to provide an objective and standardized classification protocol for urban temperature studies in any city. The field temperature data (Jul.-Sept., 2016) from 12 LCZ sites located in urban and rural areas of Nanjing, China, was used to evaluate the LCZ scheme. For the 12 LCZ sites, the features of heat island and the differences of daily max/min temperature and heating/cooling rate were analyzed. The UHI intensity increases rapidly after sunset, reaching at maximum about three to five hours later, and then declines gradually, which is the result of the variation of the heating/cooling rates of a LCZ site. It was observed that the higher level of urbanization the stronger heat island effect for the LCZ sites. The heat island magnitudes may even be negative during the midday period. It was shown that the water area (LCZ G) produces cooling effect during the daytime as expected while shows warming effects during the night time. The daily maximum temperature difference between urban and rural occurs in the minimum rather than in the maximum. Distinct differences in air temperature among the LCZ sites reflect the thermal effects of local surrounding properties.

    参考文献
    [1] STEWART I D, OKE T R. Local climate zones for urban temperature studies[J]. Bulletin of the American Meteorological Society, 2012, 93(12):1879-1900.
    [2] STEWART I D, OKE T R, KRAYENHOFF E S. Evaluation of the "local climate zone" scheme using temperature observations and model simulations[J]. International Journal of Climatology, 2014, 34(4):1062-1080.
    [3] LECONTE F, BOUYER J, CLAVERIE R, et al. Using Local Climate Zone scheme for UHI assessment:Evaluation of the method using mobile measurements[J]. Building and Environment, 2015, 83:39-49.
    [4] THOMAS G, SHERIN A P, ANSAR S, et al. Analysis of urban heat island in Kochi, India, using a modified Local Climate Zone classification[J]. Procedia Environmental Sciences, 2014, 21:3-13.
    [5] 林中立,徐涵秋. 基于LCZ的城市热岛强度研究[J]. 地球信息科学学报,2017,19(5):713-722. LIN Z L, XU H Q. A study of urban heat island intensity based on "Local Climate Zones"[J]. Journal of Geo-information Science, 2017, 19(5):713-722. (in Chinese)
    [6] 刘琳,刘京,林姚宇,等. 多种城市地表形态的局地气候分析[J]. 建筑科学,2017(2):8-14. LIU L, LIU J, LIN Y Y, et al. Local climatic analysis of multiple urban surface morphology[J]. Building Science, 2017, 33(2):8-14. (in Chinese)
    [7] 中国气象局气象信息中心气象资料室, 清华大学建筑技术科学系. 中国建筑热环境分析专用气象数据集[M]. 北京:中国建筑工业出版社, 2005. China Meteorological Bureau, Climate Information Center, Climate Data Office and Tsinghua University, Department of Building Science and Technology. China standard weather data for analyzing building thermal conditions[M]. Beijing:China Architecture & Building Press, 2005. (in Chinese)
    [8] Google earth[EB/OL].[2017-08-22]. https://earth.google.com/web/.
    [9] QI F, WANG Y. A new calculation method for shape coefficient of residential building using Google Earth[J]. Energy and Buildings, 2014, 76:72-80.
    [10] BRUSE M, FLEER H. Simulating surface-plant-air interactions inside urban environments with a three dimensional numerical model[J]. Environmental Modelling & Software, 1998, 13:373-384.
    [11] OKE T R. An algorithmic scheme to estimate hourly heat island magnitude[C]//2nd Urban Environment Symposium, 1998, Albuquerque, NM.
    [12] OKE T R. Boundary layer climates[M]. London:Routledge, 2015.
    [13] China Meteorological Data Service Center[EB/OL].[2017-06-22].http://data.cma.cn/en.
    [14] YANG X, ZHAO L. Diurnal thermal behavior of pavements, vegetation, and water pond in a hot-humid city. Buildings, 2016, 6:1-12.
    [15] CHOW W T L, ROTH M. Temporal dynamics of the urban heat island of Singapore[J]. International Journal of Climatology, 2006, 26(15):2243-2260.
    [16] SANG J, LIU H, LIU H, et al. Observational and numerical studies of wintertime urban boundary layer[J]. Jounal of Wind Engineering and Industrial Aerodynamics, 2000, 87(2):243-258.
    [17] OKE T R. The energetic basis of the urban heat island[J]. Quarterly Journal of the Royal Meteorological Society, 1982, 108:1-24.
    [18] THEEUWES N E, STEENEVELD G J, RONDA R J, et al. Cool city mornings by urban heat[J]. Environmental Research Letters, 2015:1-9.
    [19] 陈恺,唐燕. 城市局部气候分区研究进展及其在城市规划中的应用[J]. 南方建筑,2017(2):21-28. CHEN K, TANG Y. Research progress of local climate zones and its applications in urban planning[J]. South Architecture, 2017(2):21-28. (in Chinese)
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杨小山,姚灵烨,金涛,姜之点,彭立华,叶燕华.南京夏季城市局地气温时空变化特征[J].土木与环境工程学报(中英文),2019,41(1):160-167,174. Yang Xiaoshan, Yao Lingye, Jin Tao, Jiang Zhidian, Peng Lihua, Ye Yanhua. Temporal and spatial variations of local temperatures in the summer of Nanjing[J]. JOURNAL OF CIVIL AND ENVIRONMENTAL ENGINEERING,2019,41(1):160-167,174.10.11835/j. issn.2096-6717.2019.020

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  • 收稿日期:2018-06-18
  • 在线发布日期: 2019-04-04
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