###### Abstract
[14] collected satellite data from 2001 to 2003, and their study concluded that the UHI in Bangkok was equal to 8 \({}^{\circ}\)C during the dry season (November to April), 7 \({}^{\circ}\)C in Shanghai, 7 \({}^{\circ}\)C in Manila, and 12 \({}^{\circ}\)C in Tokyo. [PERSON] and [PERSON] [21] used MODIS data to investigate the UHI in Beijing, China. They found that in the summer, there is an LST differential of around 4-6 \({}^{\circ}\)C between the city and the suburbs and 8-10 \({}^{\circ}\)C between the city center and the outer suburbs. Using a combination of Advanced Spaceborne Thermal Emission, Reflection Radiometer (ASTER) and Thematic Mapper (TM) data, [PERSON] et al. [24] also discovered the UHII in Beijing from 2002 to 2006. Their findings demonstrated that urban Beijing has a high UHI effect in the summer, spring, and autumn. [PERSON] and [PERSON] [25] examined the seasonal variation in the UHII in the Delhi territory using Landsat TM data (India). They discovered that the highest UHII occurred in the summer at 16.7 \({}^{\circ}\)C when most agricultural fields were fallow and solar radiation was high. In winter, a 7.4 \({}^{\circ}\)C UHII was recorded, which was when there was low solar radiation and the farmland was covered in crops and had a lot of moisture. The second-highest UHII was observed during the monsoon season (13.8 \({}^{\circ}\)C). [PERSON] et al. [26] used MODIS data for 2003-2011 in 32 major cities in China to analyze the SUHI. They found higher SUHIIs for the day and night in the southeastern and northern regions. They noted how SUHII varied significantly depending on the season, with a higher daily intensity in the summer than in the winter and the opposite during the night for most places. [PERSON] and [PERSON] [3] proposed a classification schema LCZ (local climate zone) study of UHII in Fuzhou, China, using remote sensing technology, and the authors found that Fuzhou City's UHII LCZ on 27 September 2015, was 6.73 \({}^{\circ}\)C, indicating a worsening of the UHI in the city. The UHI in Cairo (Egypt) from 1995 to 2000 at three stations equipped with mercury thermometers was examined by [PERSON] [27]. He discovered that the urban environment was consistently drier than the suburban environment in the morning and was more humid in the afternoon. Except for November, when a chilly island developed, the urban environment was consistently warmer than its surroundings. From February to September (excluding May), the urban region was drier than the rural area, and the monthly mean UHI ranged from 1.0 \({}^{\circ}\)C to 2.2 \({}^{\circ}\)C. During the winter season, from October to January, the UHI was equivalent to approximately 1 \({}^{\circ}\)C.  
The urbanization process has increased rapidly in China due to a significant increase in economic growth. According to a report from the National Bureau of Statistics of China from 2011, urbanization increased by 13.5% in China between 2000 and the end of 2010, increasing the UHI effects [9; 28; 29; 30]. A study conducted by [PERSON] et al. examined the evolution of urban heat islands and vegetation coverage in Zhengzhou City [31]. The findings show that during the past 15 years (2006-2020), a high-temperature zone in the urban area has gradually spread to the nearby districts, worsening the urban heat island as a whole. The heat island area initially increased by 138.72 km\({}^{2}\) between 2006 and 2014. In order to examine the intensity of the UHI in Zhengzhou, China, over a 39-year period (1981-2019), [PERSON] et al. conducted a study that used long-term observation and statistical data on annual, seasonal, daytime, and nighttime bases [32]. The associations between UHI and signs of rapid urbanization, as well as the temporal variations in the UHI effect, were also examined in this study. According to the findings, Zhengzhou is warming at a rate that is 2.2 times faster than the approximate +0.9 \({}^{\circ}\)C average for land warming between 1981 and 2019.