2005-2020年逐年1Km中国夏季地表城市热岛空间数据集及空间扩张分析OA北大核心CSTPCD
Annual 1-kilometer spatial dataset of summer urban heat island and spatial expansion analysis in China from 2005 to 2020
在全球气候变暖和城市化进程加速的背景下,城市热岛效应日益加剧.本研究耦合地表温度、土地利用覆被、城市建成区边界和数字高程模型等数据,基于GEE(Google Earth Engine)平台对逐8天MODIS LST(Land Surface Temperature)产品进行时间线性插值并生产全国无缝LST数据,进一步利用动态简化城市边界算法,研发2005-2020年逐年1 km空间分辨率中国夏季地表城市热岛空间数据集.在此基础上,使用城市热岛空间扩张指数揭示2005-2020年夏季昼夜中国城市热岛空间扩张特征.研究结果表明,2005-2020年夏季昼夜中国地表城市热岛面积分别增长1.95和2.49倍.2020年夏季昼夜中国地表城市热岛强度分别为1.36℃和1.33℃,较2005年增长0.08℃和0.38℃.2005-2020年夏季昼夜中国地表城市热岛空间扩张均以边缘型为主,2015-2020年城市热岛空间扩张程度在各时期最高.填充型城市热岛空间扩张城市热岛强度最高.本研究所研发的时间线性插值算法和动态简化城市边界算法为长时间序列城市热岛效应空间识别和城市热岛强度表征提供技术范式,中国地表城市热岛空间数据集为主动适应和减缓城市热环境风险与促进城市可持续发展提供数据支持.
The Earth's climate system is undergoing global climate change characterized by warming,which is influenced by both natural climate and human activities.In the context of global warming and accelerated urbanization,extreme climate risks such as heat waves are intensifying,leading to serious consequences such as deaths.As an important manifestation of the disturbance of the Earth's climate system,Urban Heat Island(UHI)is a typical phenomenon of the combined effects of global climate change and human activities.Therefore,establishing a long time series and high spatiotemporal resolution dataset of UHI effects is of great scientific significance and practical value for establishing a systematic high-temperature response framework,such as high-temperature response plans,mitigation and adaptation guidelines,decision support systems,policy incentive guidelines,etc. This study coupled data of land surface temperature,land use and cover,urban built-up boundary,and digital elevation model,and based on the Google Earth Engine(GEE)platform,performed a temporal linear interpolation on the 8-day MODIS LST(Land Surface Temperature)product,filled the missing data of MODIS from the temporal dimension,and used the values obtained by the temporal linear interpolation to fill the missing values,which are the average temperatures of the adjacent times under the missing values,producing a seamless LST data for the whole country.Furthermore,using a dynamic simplified urban boundary algorithm,within the urban built-up boundary,according to the different types of land use and cover,the urban built-up areas and water bodies such as rivers were excluded,and the cases with large differences in digital elevation were also excluded,obtaining the rural areas,and then calculating the average rural temperature,and then using the average rural temperature as the background,calculating the UHI intensity according to the temperature within the urban built-up boundary,obtaining a spatial dataset of summer land surface UHI in China with an annual 1 km spatial resolution from 2005 to 2020.And according to the morphological relationship of UHI changes,the UHI morphological changes were expressed by the UHI spatial expansion index,and according to the size of the index,they were divided into edge type,filled type,and enclave type,and finally the spatial expansion characteristics of the summer day and night UHI in China from 2005 to 2020 were revealed by the UHI spatial expansion index. The research results show that the summer daytime and nighttime land surface UHI area in China increased by 1.95 and 2.49 times,respectively,from 2005 to 2020.The summer daytime and nighttime land surface UHI intensity in China in 2020 were 1.36°C and 1.33°C,respectively,an increase of 0.08°C and 0.38°C compared to 2005.The UHI intensity is relatively stable in the eastern region,but high and fluctuates greatly in the western region.In summer 2005,the surface UHI intensity was higher during daytime than at night.In summer 2020,the nighttime surface UHI intensity increased significantly,especially in the central and eastern regions,which was higher than the daytime surface UHI intensity.The spatial expansion of the summer daytime and nighttime land surface UHI in China from 2005 to 2020 was dominated by the edge type,and the degree of UHI spatial expansion was the highest in 2015-2020.The filled type UHI spatial expansion had the highest UHI intensity.This study used the land surface temperature temporal linear interpolation algorithm,which improved the temporal accuracy of the original MODIS LST temperature data,ensuring that the land surface temperature data had no missing data,and used the GUB data of multiple years to identify the UHI effects of the corresponding years,and dynamically updating the GUB data was the most important guarantee for improving the spatial identification accuracy of the UHI effects.And based on the research,it proposed to use the spatiotemporal interpolation algorithm and annual GUB data to further improve the accuracy of the spatial dataset of UHI in China. The temporal linear interpolation algorithm and the dynamic simplified urban boundary algorithm used in this study provide a technical paradigm for the quantitative identification of UHI effects in long time series,and the spatial dataset of land surface UHI in China provides data support for actively adapting and mitigating urban thermal environmental risks and promoting urban sustainable development.
贾若愚;刘洛;徐新良;韩冬锐;乔治
天津大学环境科学与工程学院华南农业大学资源环境学院学院中国科学院地理科学与资源研究所山东省农业科学院农业信息与经济研究所天津大学环境科学与工程学院
土木建筑
城市热岛效应地表温度时间线性插值动态简化城市边界算法空间扩张GEE
urban heat islandland surface temperaturetime linear interpolationdynamic simplified urban-extent algorithmspatial expansiongoogle earth engine
《西部人居环境学刊》 2024 (6)
149-154,6
国家自然科学基金项目(52270187)天津市自然科学基金项目(21JCYBJC00390)
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