SPATIAL VARIATION OF THE CHRACTERISTICS OF URBAN HEAT ISLAND EFFECT IN HONG KONG

被引:0
作者
Mok, H. Y. [1 ]
Wu, M. C. [1 ]
Cheng, C. Y. [1 ]
机构
[1] Hong Kong Observ, Kowloon, Hong Kong, Peoples R China
来源
PROCEEDINGS OF THE FIRST INTERNATIONAL CONFERENCE ON SUSTAINABLE URBANIZATION (ICSU 2010) | 2010年
关键词
Hong Kong; Urban Heat Island; heating rates; cooling rates; diurnal temperature ranges;
D O I
暂无
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Recent studies by the Hong Kong Observatory show that the urban centre of Hong Kong has considerable Urban Heat Island (UHI) effect that arises from the different thermal properties between urban and the surrounding rural areas. The studies have also shown that the urban-rural temperature difference or UHI intensity in the urban centre of Hong Kong can be greater than 10 degrees C. However, the characteristics of UHI in Hong Kong would not be unique were it not for its complex topography and the significant spatial variation in the degree of urbanization within the territory. Making use of the extensive spatial coverage of the automatic weather stations operated by the Observatory, this study attempts to document the spatial variation of the characteristics of UHI effect in Hong Kong in summer and winter through cases studies. Cases in summer and winter with meteorological conditions typical for high UHI effect (that is, clear sky, light wind and stable atmospheric condition) are selected for the study. The characteristics of UHI effect in terms of the daytime warming rates, nocturnal cooling rates and diurnal temperature ranges at the selected automatic weather stations are analysed. The territory of Hong Kong is then classified into different categories according to the identified characteristics with a view to portraying the spatial morphology of UHI effect in Hong Kong.
引用
收藏
页码:494 / 500
页数:7
相关论文
共 22 条
[1]  
Alonso MS, 2003, ATMOSFERA, V16, P137
[2]   Two decades of urban climate research: A review of turbulence, exchanges of energy and water, and the urban heat island [J].
Arnfield, AJ .
INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2003, 23 (01) :1-26
[3]   A canopy layer model and its application to Rome [J].
Bonacquisti, V. ;
Casale, G. R. ;
Palmieri, S. ;
Siani, A. M. .
SCIENCE OF THE TOTAL ENVIRONMENT, 2006, 364 (1-3) :1-13
[4]  
Chang W.L., 1997, 840 WMOTD
[5]   Mesoscale aspects of the Urban Heat Island around New York City [J].
Gedzelman, SD ;
Austin, S ;
Cermak, R ;
Stefano, N ;
Partridge, S ;
Quesenberry, S ;
Robinson, DA .
THEORETICAL AND APPLIED CLIMATOLOGY, 2003, 75 (1-2) :29-42
[6]   Daytime urban heat island effect in high-rise and high-density residential developments in Hong Kong [J].
Giridharan, R ;
Ganesan, S ;
Lau, SSY .
ENERGY AND BUILDINGS, 2004, 36 (06) :525-534
[7]  
Gonzalez J.E., 2005, Eos, Transactions American Geophysical Union, V86, P397, DOI [DOI 10.1029/2005E0420001, 10.1029/2005EO420001, DOI 10.1029/2005EO420001]
[8]  
Gonzalez J.E., 2005, EOS Transactions, AGU, V42, P403
[9]   Scaling the Daytime Urban Heat Island and Urban-Breeze Circulation [J].
Hidalgo, Julia ;
Masson, Valery ;
Gimeno, Luis .
JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY, 2010, 49 (05) :889-901
[10]   Spatial and temporal structure of the urban heat island in Seoul [J].
Kim, YH ;
Baik, JJ .
JOURNAL OF APPLIED METEOROLOGY, 2005, 44 (05) :591-605