Surface urban heat island in China's 32 major cities: Spatial patterns and drivers

被引:591
|
作者
Zhou, Decheng [1 ,2 ]
Zhao, Shuqing [1 ,2 ]
Liu, Shuguang [3 ,4 ]
Zhang, Liangxia [5 ]
Zhu, Chao [1 ,2 ]
机构
[1] Peking Univ, Coll Urban & Environm Sci, Beijing 100871, Peoples R China
[2] Peking Univ, Key Lab Earth Surface Proc, Minist Educ, Beijing 100871, Peoples R China
[3] Natl Engn Lab Forest Ecol & Appl Technol Southern, Changsha 410004, Hunan, Peoples R China
[4] Cent South Univ Forest & Technol, Changsha 410004, Hunan, Peoples R China
[5] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
基金
湖南省自然科学基金; 中国国家自然科学基金;
关键词
urbanization; land surface temperature (LST); spatial variations; driving forces; enhanced vegetation index (EVI); albedo; climatic effects; LAND-SURFACE; IMPERVIOUS SURFACE; NIGHTTIME LIGHTS; CLIMATE-CHANGE; AIR-POLLUTION; COVER CHANGE; TEMPERATURE; ENERGY; MODIS; CITY;
D O I
10.1016/j.rse.2014.05.017
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Urban heat island (UHI) is a major anthropogenic alteration on Earth environments and its geospatial pattern remains poorly understood over large areas. Using MODIS data from 2003 to 2011, we quantified the diurnal and seasonal surface UHI intensity (SUHII, urban-suburban temperature difference) in China's 32 major cities, and analyzed their spatial variations and possible underlying mechanisms. Results show that the annual mean SUHII varied markedly from 0.01 to 1.87 degrees C in the day and 035 to 1.95 degrees C at night, with a great deal of spatial heterogeneities. Higher SUHIls for the day and night were observed in the southeastern and northern regions, respectively. Moreover, the SUHII differed greatly by season, characterized by a higher intensity in summer than in winter during the day, and the opposite during the night for most cities. Consequently, whether the daytime SUHII was higher or lower than the nighttime SUHII for a city depends strongly on the geographic location and research period. The SUHII's distribution in the day related closely to vegetation activity and anthropogenic heat releases in summer, and to climate (temperature and precipitation) in winter, while that at night linked tightly to albedo, anthropogenic heat releases, built-up intensity, and climate in both seasons. Overall, we found the overwhelming control of climate on the SUHII's spatial variability, yet the factors included in this study explained a much smaller fraction of the SUHII variations in the day compared to night and in summer relative to winter (day vs. night: 57% vs. 72% in summer, and 61% vs. 90% in winter, respectively), indicating more complicated mechanisms underlying the distribution of daytime SUHII, particularly in summer. Our results highlight the different diurnal (day and night) and seasonal (summer and winter) SUHII's spatial patterns and driving forces, suggesting various strategies are needed for an effective UHI effect mitigation. (C) 2014 Elsevier Inc. All rights reserved.
引用
收藏
页码:51 / 61
页数:11
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