Shi Kaifang, Wu Yizhen, Liu Shirao
Key Laboratory of Earth Surface Processes and Regional Response in the Yangtze-Huaihe River Basin, Anhui Province, School of Geography and Tourism, Anhui Normal University, 241002, China; Chongqing Jinfo Mountain Karst Ecosystem National Observation and Research Station, School of Geographical Sciences, Southwest University, Chongqing, 400715, China; Chongqing Engineering Research Centre for Remote Sensing Big Data Application, School of Geographical Sciences, Southwest University, Chongqing, 400715, China.
Key Laboratory of Earth Surface Processes and Regional Response in the Yangtze-Huaihe River Basin, Anhui Province, School of Geography and Tourism, Anhui Normal University, 241002, China; Chongqing Jinfo Mountain Karst Ecosystem National Observation and Research Station, School of Geographical Sciences, Southwest University, Chongqing, 400715, China; Chongqing Engineering Research Centre for Remote Sensing Big Data Application, School of Geographical Sciences, Southwest University, Chongqing, 400715, China.
J Environ Manage. 2022 Dec 15;324:116337. doi: 10.1016/j.jenvman.2022.116337. Epub 2022 Oct 12.
The tendency of global urban expansion to be slope climbing has partly become possible with scarce cropland resources in plains. However, the scientific understanding of the quantity, intensity, pattern, and effect of the slope climbing of urban expansion (SCE) is minimal globally. In this study, we have attempted to quantify and evaluate global SCE from Suomi National Polar-orbiting Partnership (SNPP)-Visible Infrared Imaging Radiometer Suite (VIIRS)-like data and other auxiliary data. Results revealed that global SCE areas unevenly increased from 22,760 km to 90,720 km from 2000 to 2020, with an annual growth rate of 21.72%, in which low-environment cost type areas increased from 21,550 km to 84,010 km while high-environment cost type (HEC) areas increased from 1210 km to 6710 km. One remarkable phenomenon is that China's SCE areas in 2020 were more than 11 times those in 2000. In addition, global SCE intensity increased by about 3.4-fold from 2000 to 2020 and the rapid growth of HEC intensity is concentrated in Asia and North America. SCE is mostly affected by urban population growth and terrain. Economic development also promotes its development to a certain extent. We also noted that global SCE potentially made a considerable contribution to saved cropland, saving about 46,747 km with a theoretical increased grain yield of 25,020 × 10 t. Our study provides timely and transparent monitoring of global SCE and offers new insights into sustainable urban development.
由于平原地区耕地资源稀缺,全球城市扩张呈现爬坡趋势在一定程度上成为可能。然而,全球范围内对城市扩张爬坡(SCE)的数量、强度、模式和影响的科学认识仍极为有限。在本研究中,我们尝试从类似苏米国家极地轨道伙伴计划(SNPP)-可见红外成像辐射仪套件(VIIRS)的数据及其他辅助数据中对全球SCE进行量化和评估。结果显示,2000年至2020年期间,全球SCE面积从22760平方千米不均衡地增加到90720平方千米,年增长率为21.72%,其中低环境成本类型区域从21550平方千米增加到84010平方千米,而高环境成本类型(HEC)区域从1210平方千米增加到6710平方千米。一个显著现象是,2020年中国的SCE面积是2000年的11倍多。此外,2000年至2020年期间,全球SCE强度增加了约3.4倍,HEC强度的快速增长集中在亚洲和北美洲。SCE主要受城市人口增长和地形的影响。经济发展在一定程度上也推动了其发展。我们还注意到,全球SCE可能为节省耕地做出了相当大的贡献,节省了约46747平方千米的耕地,理论上粮食产量增加了25020×10吨。我们的研究为全球SCE提供了及时且透明的监测,并为可持续城市发展提供了新的见解。