生态与农村环境学报

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基于地理探测器的喀什市地表热场空间分异及影响因素分析

赵禾苗;阿里木江·卡斯木   

  • 基金资助:
    国家自然科学基金(41661037)

Analysis of Spatial Differentiation and Influencing Factors of Surface Thermal Field in Kashgar City Based on Geographic Detector

ZHAO He-miao; ALIMUJIANG Kasimu   

摘要: 科学认识城市地表热场时空格局及驱动因子是优化城市生态系统的重要前提。喀什市是东西方文明与交通的咽喉枢纽,地处帕米尔高原北麓,在“一带一路”倡议中的战略位置至关重要。以绿洲城市喀什市为例,借助GIS和RS技术支持,在利用辐射传输方程法对地表温度(LST)进行反演的基础上,提取不透水面指数(IBI)和植被覆盖度(FVC),运用空间转移矩阵分析喀什市地表温度空间分异状况,综合海拔、坡度、人口密度、IBI、FVC和土地利用类型6类影响因子,应用地理探测器对喀什市近20 a间地表热场空间异质性与驱动因子进行探测。结果表明:(1)在空间尺度上,中温区与较高温区连片分布于城市建成区,低温与较低温区呈点状镶嵌于建成区外围,高温与特高温区成片分布于市区北部的裸地处。(2)在时间尺度上,伴随区域不断开发,中温区逐渐占据主导地位,至2018年,温区面积为161.89km2,占比达29.45%;由于“侵占耕地,扩展城镇”与“植树造林”现象同时存在,低温区增加了4.58%,裸地得到有效改善,高温与特高温区面积减少20.41 km。(3)喀什市地表热环境空间分异是多因素共同作用的结果,影响LST空间分异的核心因素是IBI,1998、2008和2018年的贡献率分别为87.8%、74.6%、80.8%,同时多因子交互作用明显,IBI与土地利用类型1998、2008和2018年的交互解释力分别达0.912、0.746、0.873。研究结果可为喀什市城市生态保护和区域可持续发展提供参考依据。

关键词: 地表温度(LST), 地理探测器, 空间转移矩阵, 喀什市

Abstract: Scientific understanding of the temporal and spatial patterns and driving factors of urban surface thermal fields is an important prerequisite for optimizing urban ecosystems. Kashgar City is the throat hub of civilization and transportation between the East and the West, and its strategic position in the "Belt and Road" is very important. In this paper, the Landsat series of remote sensing images in 1998, 2008, and 2018 of the city of Kashgar on the western edge of the Tarim Basin have been used. The land surface temperature was retrieved with the radiative transfer equation algorithm and to analyze the spatial variation of surface temperature in Kashgar City by using transfer matrix with the help of “GIS” and “RS” technology. Next, on the basis of extracting impervious surface index and vegetation coverage, 6 types of influencing factors including altitude, slope, population density, IBI, FVC and land use type are integrated to detect the spatial heterogeneity and driving factors of the surface thermal field with geographic detectors in Kashgar City in the past 20 years.The results showed as follows: First, the middle temperature area and the higher temperature area are contiguously distributed in the urban built-up area, the low temperature and the lower temperature area are inlaid in the periphery of the built area in dots, and the high temperature and extremely high temperature areas are distributed in patches in the north of the urban area. Second, with the continuous development of the region, the medium temperature zone gradually dominates. In 2018, the temperature zone area was 161.89 km2, meanwhile, duing to the coexistence of the phenomenon of "invading cultivated land and expanding towns" and "forestation", the low temperature zone increased by 4.58 %, the bare land is effectively improved, and the area of the high temperature and ultra-high temperature zone is reduced by 20.41km2. Last, the spatial differentiation of the surface thermal environment in Kashgar is the result of multiple factors. The core factor affecting the spatial differentiation of LST is IBI. The three-year contribution rates are 87.8%, 74.6%, and 80.8%, and the multi-factor interaction is obvious. The interactive explanatory powers of IBI and land use types in 1998, 2008 and 2018 were 0.912, 0.746, and 0.873, respectively. The research results can provide reference for urban ecological protection and regional sustainable development in Kashgar City.

Key words: land surface temperature, geographical detector, conversion matrix, Kashgar city

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