2021
DOI: 10.1016/j.ecolind.2020.107230
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Simulation of future land surface temperature distribution and evaluating surface urban heat island based on impervious surface area

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Cited by 78 publications
(32 citation statements)
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“…The area of tree-based green space within approximately 0.32 ha can effectively enhance their cooling intensity [30]. A high coverage ratio of green space corresponds to a lower surface temperature [31,32]. Belt-shaped green areas parallel to the wind direction appear to have a higher cooling effect than those vertical to the wind direction and the difference of the cooling effect reached 6.3 K between the two orientation scenarios with big canopy trees [33].…”
Section: Introductionmentioning
confidence: 99%
“…The area of tree-based green space within approximately 0.32 ha can effectively enhance their cooling intensity [30]. A high coverage ratio of green space corresponds to a lower surface temperature [31,32]. Belt-shaped green areas parallel to the wind direction appear to have a higher cooling effect than those vertical to the wind direction and the difference of the cooling effect reached 6.3 K between the two orientation scenarios with big canopy trees [33].…”
Section: Introductionmentioning
confidence: 99%
“…The first was the change in surface radiation energy balance. In humid and semi-humid regions, the change in bare soil was relatively small, and the expansion of impervious surface area and loss of vegetation space were the main land change, which brought about an increase in land surface temperature and was easy to form urban heat island phenomena [58,59] due to the perceived energy change by the human body from impervious surface area to vegetation space. In contrast, in arid and semi-arid regions, the type of land change within the urban areas was dominated by both the expansion of impervious surface area and vegetation space and the loss of bare soil.…”
Section: Potential Environmental Effects Of Intra-urban Land Change In Africa During 2000-2020mentioning
confidence: 99%
“…Nevertheless, the rapid development of remote sensing techniques has enabled satellite images to acquire near-real-time data on detailed spatial surfaces. Therefore, to obtain high-resolution, consistent, and repetitive LST at the regional and global scales, remote sensing is the only practical and feasible way [ 8 , 9 , 10 , 11 , 12 ]. Many satellites carry thermal infrared sensors, such as MODIS/Terra and Aqua, advanced very high-resolution radiometer (AVHRR)/NOAA, and Landsat-8/TIRS [ 13 ].…”
Section: Introductionmentioning
confidence: 99%