Spatial and temporal structure of the urban heat island in Seoul

被引:240
作者
Kim, YH
Baik, JJ [1 ]
机构
[1] Seoul Natl Univ, Sch Earth & Environm Sci, Seoul 151742, South Korea
[2] Korea Meteorl Adm, Met Res Inst, Seoul, South Korea
来源
JOURNAL OF APPLIED METEOROLOGY | 2005年 / 44卷 / 05期
关键词
D O I
10.1175/JAM2226.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The spatial and temporal structure of the urban heat island in Seoul, Korea, is investigated using near-surface temperature data measured at 31 automatic weather stations (AWSs) in the Seoul metropolitan area for the 1-yr period from March 2001 to February 2002. The urban heat island in Seoul deviates considerably from an idealized, concentric heat island structure, mainly because of the location of the main commercial and industrial sectors and the local topography. Relatively warm regions extend in the east-west direction and relatively cold regions are located near the,northern and southern mountains. Several warm cores are observed whose intensity, size, and location are found to vary seasonally and diurnally. Similar to previous studies, the urban heat island in Seoul is stronger in the nighttime than in the daytime and decreases with increasing wind speed and cloud cover, but it is least developed in summer. The average maximum urban heat island intensity is 2.2 degrees C over the 1-yr period and it is 3.4 degrees C at 0300 local standard time (LST) and 0.6 degrees C at 1500 LST. The reversed urban heat island is occasionally observed in the afternoon, but its intensity is very weak. An empirical orthogonal function (EOF) analysis is performed to find the dominant modes of variability in the Seoul urban heat island. In the analysis using temperature data that are averaged for each hour of the 1-yr period, the first EOF explains 80.6% of the total variance and is a major diurnal mode. The second EOF, whose horizontal structure is positive in the eastern part of Seoul and is negative in the western part, explains 16.0% of the total variance. This mode is related to the land use type and the diurnal pattern of anthropogenic heat release. In the analysis using temperature data at 0300 LST, the leading four modes explain 72.4% of the total variance. The first EOF reflects that the weakest urban heat island intensity is in summer. It is found that the urban heat island in Seoul is stronger on weekdays than weekends.
引用
收藏
页码:591 / 605
页数:15
相关论文
共 40 条
[1]   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
[2]  
Baik JJ, 2001, J APPL METEOROL, V40, P1462, DOI 10.1175/1520-0450(2001)040<1462:DAMCFB>2.0.CO
[3]  
2
[4]  
BOO KO, 2000, J KOREAN METEOR SOC, V36, P499
[5]   A multiple linear statistical model for estimating the mean maximum urban heat island [J].
Bottyán, Z ;
Unger, J .
THEORETICAL AND APPLIED CLIMATOLOGY, 2003, 75 (3-4) :233-243
[6]  
BYUN DW, 1987, THESIS N CAROLINA ST
[7]  
CHANGNON SA, 1981, METEOR MONOGR AM MET, V40
[8]  
Cotton W.R., 1995, Human impacts on weather and climate
[9]   Impact of rapid urban growth on heat and moisture islands in Pune City, India [J].
Deosthali, V .
ATMOSPHERIC ENVIRONMENT, 2000, 34 (17) :2745-2754
[10]  
DRAXLER RR, 1986, J CLIM APPL METEOROL, V25, P1125, DOI 10.1175/1520-0450(1986)025<1125:SAOIOT>2.0.CO