[Thermal Environment Evolution and Response Mechanism of Urban Sprawl Based on Multi-source Data].

Improving the urban thermal environment and improving the quality of human settlements are important prerequisites for creating ecologically livable cities. The current research on the relationship between urban expansion and the thermal environment is mostly based on remote sensing data, and the application of multi-source data is weak. Here, we selected the Xi'an metropolitan core area, measured the urban expansion and temporal and spatial evolution of the thermal environment based on Landsat remote sensing images in 2010 and 2020, and used multi-source data, such as interest points and the Baidu thermal index, to study the response mechanism of the urban thermal environment through geoscience statistical analysis methods. The results showed that:① the construction land in the study area had expanded by 200.84 km2, and the area and intensity showed that "the center and the periphery are weaker, and the difference between the two" characteristics, and the expansion mode was mainly edge type and infill type. ② Between 2010 and 2020, the overall thermal environment in the study area deteriorated, and the area of the heat island area increased by 282.65 km2. The spread of the heat island area was in the same direction as the urban expansion, and the distribution pattern evolved from "southeast-northwest" to "northeast-southwest;" however, the average temperature in the central area of the city decreased 1.09℃. ③ Urban expansion was strongly positively correlated with the deterioration of the urban thermal environment. The expansion of urban space had a contribution rate of 60.40% to the deterioration of the thermal environment, and various socio-economic factors had a weaker effect, with an overall contribution rate of 39.60%. The vegetation water body had an obvious cooling effect; under the influence of multiple factors, the surface temperature increased by 0.241 units. In the process of urban expansion, changes in surface parameters and two-dimensional urban morphology were still the main factors for thermal environment changes, whereas three-dimensional morphology had a small effect on the warming of social and economic activities, and the contribution of water bodies and vegetation to cooling was prominent.