Thai Nguyen City, strategically located in the northern region of Vietnam between the coordinates 21°28'48"-21°37' 22"N and 105°42'3"-105°54'54"E, holds immense significance as a hub for economic and social advancement within Thai Nguyen province (Fig 1). It plays a pivotal role in the comprehensive socio-economic development strategy of the northern economic region of Vietnam, as highlighted by
Le and Nguyen (2022). With a sprawling land area of 222.93 km², Thai Nguyen City has evolved into a vibrant urban center, accommodating an approximate population of 362,921 individuals as of 2021 (
Le and Nguyen, 2022). The city experiences a humid subtropical climate characterized by four distinct seasons that include spring, summer, autumn and winter. These seasonal variations contribute to the diversity and richness of the city’s natural environment. The average temperatures in Thai Nguyen City hover around 22.4°C, allowing for comfortable living conditions throughout the year (
Le and Nguyen, 2022). Moreover, the region receives an average annual rainfall ranging from 2,000 to 2,500 mm
(Phung et al., 2019). This generous rainfall sustains the lush greenery and contributes to the overall ecological balance of the area. Thai Nguyen City’s geographical location and favorable climate provide a solid foundation for its economic growth and development
(Phung et al., 2019). The city serves as a thriving center for various industries, including manufacturing, textiles and metallurgy (
Le and Nguyen, 2022). Its strategic position within the northern economic region of Vietnam positions Thai Nguyen City as a key contributor to the region’s economic progress
(Phung et al., 2019).
The study utilized satellite imagery from different sources and periods to assess the VCA changes. Landsat 5 TM (Thematic Mapper) images for May 2001 and 2010 were obtained from the United States Geological Survey (USGS) Earth Explorer website (
https://glovis.usgs.gov). Sentinel 2A images for May 2023 were acquired from the Open Access Hub (https://scihub.copernicus.eu) (Table 1) (
Congedo, 2021;
Zhang et al., 2021). All satellite images underwent geometric correction and rectification to UTM zone 48N. To analyze the VCA over time, the RDAS IMAGINE 2020 software (Version 16.6) was used. In addition, ArcGIS (Version 10.2) played a role in digitizing, indexing, image analysis, geo-referencing and database creation (
Deval and Joshi, 2022;
Huang et al., 2021). The combination of these software tools enabled efficient handling and processing of satellite imagery data, ensuring accurate results
(Thakkar et al., 2016; Zhang et al., 2021).
To ensure reliable and accurate analysis of the digital images, a thorough process of geometric and radiometric calibration was conducted
(Thakkar et al., 2016). Geometric rectification, in particular, plays a crucial role in detecting VCA. By precisely aligning the pixels of multi-temporal remote sensing data, it minimizes the risk of misinterpreting registration errors as VCA (
Congedo, 2021;
Thakkar et al., 2016). Geometric rectification is essential for achieving consistency and facilitating the comparison of images over time. It ensures that each pixel is accurately registered, allowing for a reliable assessment of actual vegetation cover changes. By eliminating discrepancies caused by misalignment, the analysis can provide valuable insights into the dynamics of the VCA. The meticulous calibration process guarantees the integrity and consistency of the digital images, enhancing the accuracy of the subsequent analysis. It enables researchers to confidently identify and quantify changes in the VCA, contributing to a better understanding of the evolving vegetation patterns and their underlying factors. The application of geometric rectification techniques is therefore a fundamental step in conducting comprehensive and reliable studies of vegetation dynamics.
In this study, the NDVI approach, widely used in VCA studies, was employed
(Huang et al., 2021; Jeevalakshmi et al., 2016). The NDVI calculates the normalized ratio of red and near-infrared reflectance, which has proven to be effective in detecting VCA over time
(Bhandari et al., 2012). To classify pixels with unknown identity, a supervised classification process was implemented, utilizing marked samples of known identity
(Bhandari et al., 2012; Jeevalakshmi et al., 2016). This process aimed to quantify the amount of vegetation and compare vegetation levels between two different periods. The NDVI values theoretically range from -1 to 1 and different land cover types are associated with specific ranges
(Huang et al., 2021; Jeevalakshmi et al., 2016). Extremely negative NDVI values typically correspond to water bodies and built-up areas, while values ranging from 0.006 to 0.467 indicate areas of bare land or non-vegetated surfaces
(Jeevalakshmi et al., 2016). NDVI values close to zero and up to 0.657 represent varying levels of vegetation cover, including both sparse and dense vegetation (Table 2). By analyzing the NDVI values, the study aimed to assess and characterize the VCA, providing valuable insights into the dynamics of the studied area.