Urban expansion, one of the basic characteristics of urbanization, is considered an important factor influencing the natural urban ecosystem. Urban expansion inevitably causes land cover changes, shown by the rapid conversion from natural cover to artificial cover (
Kuang, 2012). Therefore, precise spatial and temporal dynamic information regarding urban land cover is required to understand the dynamics of the mechanism of the effect of urbanization within the regional ecosystem evolution. Land-Use and Land-Cover Change (LUCC) data is used for most research on urban expansion. However, the land cover changes brought about by urban expansions are generally shown by gradient features, rendering it impossible to use Land-Use and Land-Cover Change to effectively identify inner heterogeneous characteristics of the same land cover type. Changes in the impervious surface are the main indicators of urban expansion. Urban impervious surfaces refer to the artificial materials that water cannot penetrate to soil. For impervious surface, a continuous value of 0-1 is used to represent the percentage of impervious surface in each pixel. Impervious surfaces, a typical land cover constituent, can effectively describe the spatial gradient features of land cover changes (Ridd 1995;
Li and Wu, 2016). It is a significant indicative factor for urban environmental quality and urban ecosystems, and its growth is closely related to driving factors such as urban development strategic targets and overall urban planning, significantly effecting the sound sustainable development of a city (
Wang, 2013). Impervious surface produces a direct effect on regional vertical radiation balance through changes in surface albedo, emissivity, and surface roughness. This is caused by changes within the urban surface structure, thereby aggravating the surface sensible heat flux and heat island intensity, changing the regional climate, and affecting urban ecosystem service functions, particularly the thermal regulation function (
Haashemi et al., 2016). Concurrently, urban impervious surfaces exhibit poor water storage capacity and obstruct air current transmission, resulting in substantial eco-environmental element effects, such as the urban land surface hydrological cycle, non-point source pollution, and biodiversity, thus becoming an important cause of urban eco-environmental changes. Yang and Liu (2005) and Yang (2006) have utilized the urban impervious surface to analyze the speed and spatial features of urban growth and have suggested that urban impervious surface information indicates urban expansion. Weng (2004) and Hao (2016) demonstrated that distribution of the urban impervious surface has an important relationship with the urban heat island effect. In addition to being used to measure the natural environment and ecological health, the urban impervious surface also reflects the urban inner structure, which is closely linked with urban social and humanistic conditions (
Weng et al., 2009;
Yuan and Bauer, 2007). Wu and Murray (2005, 2007) have utilized urban impervious surface information to estimate the detailed distribution information of residential population of a city. Yu and Wu (2004) demonstrated that urban impervious surface information can reflect quality of living and have used it to study urban population isolation. Research by Yu and Wu (2006) found that the urban impervious surface has certain effects on housing prices. Therefore, the extraction of urban impervious surface information has become a hot topic, with research on dynamic changes in the urban impervious surface being of great practical significance.