State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; University of Chinese Academy of Sciences, Beijing 100049, China.
State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; University of Chinese Academy of Sciences, Beijing 100049, China; Beijing Urban Ecosystem Research Station, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China.
Sci Total Environ. 2021 Oct 15;791:148334. doi: 10.1016/j.scitotenv.2021.148334. Epub 2021 Jun 7.
Intensity of urban heat island (UHII) is a key indicator to quantify the magnitude of UHI effect. Change in UHII, however, can be affected by change in urban or rural temperature, or both. Numerous studies have investigated the change of UHII, but how it relates to change in urban and rural temperature is poorly understood. Here we present a continental scale analysis on the change in UHII from 2000 to 2015 in 31 major cities in China, and further explored whether such change was caused by urban warming. We used time series analysis based on MODIS land surface temperature product (MOD11A2) in summer. We found: (1) A majority of the cities (25 out of 31) had an increasing trend in UHII from 2000 to 2015, among which 44% were significant, suggesting a significantly intensified UHI effects. (2) Intensified UHII does not necessarily mean deterioration of urban thermal environment, and vice versa. For the 25 cities with an increasing trend in UHII, 11 cities had a decreasing trend of LST in both urban and rural areas. Meanwhile, for the 6 cities with a decreasing trend in UHII, three had warming trend in both urban and rural areas. (3) The attribution of changes in UHII to that of urban and rural LST indicated that it is necessary to quantify the change of LST in both urban and rural areas to fully quantify the impact of urbanization on UHI effect.
城市热岛强度(UHII)是量化热岛效应程度的关键指标。然而,UHII 的变化可能受到城市或农村温度变化的影响,或者两者都有影响。许多研究都调查了 UHII 的变化,但它与城市和农村温度变化的关系还不太清楚。在这里,我们对中国 31 个主要城市 2000 年至 2015 年期间 UHII 的变化进行了大陆尺度的分析,并进一步探讨了这种变化是否是由城市变暖引起的。我们使用基于 MODIS 地表温度产品(MOD11A2)的夏季时间序列分析。我们发现:(1)大多数城市(31 个中的 25 个)在 2000 年至 2015 年间 UHII 呈上升趋势,其中 44%具有显著意义,这表明热岛效应明显加剧。(2)加剧的 UHII 并不一定意味着城市热环境恶化,反之亦然。在 25 个 UHII 呈上升趋势的城市中,有 11 个城市城乡 LST 呈下降趋势。同时,在 6 个 UHII 呈下降趋势的城市中,有 3 个城市城乡 LST 呈变暖趋势。(3)UHII 变化归因于城乡 LST 的变化表明,有必要量化城乡 LST 的变化,以充分量化城市化对热岛效应的影响。