ECO-GEOGRAPHICAL MAPPING OF URBAN GREEN BIOMASS DYNAMICS USING NDVI, EVI, AND LAND SURFACE TEMPERATURE: A CASE STUDY OF TASHKENT
Abstract
Urban green biomass plays a critical role in regulating the ecological and thermal environment of rapidly urbanizing cities. This study aims to assess the spatio-temporal dynamics of urban green biomass and its relationship with land surface temperature (LST) in Tashkent using remote sensing techniques. Multispectral satellite data from Landsat 8/9 were processed within the Google Earth Engine platform for the period 2015–2025. Vegetation indices, including the Normalized Difference Vegetation Index (NDVI) and Enhanced Vegetation Index (EVI), were calculated to quantify green biomass distribution and dynamics. Additionally, LST was derived to evaluate the thermal environment of the study area. The results indicate a general decreasing trend in NDVI and EVI values over the study period, suggesting a gradual reduction in urban green biomass. In contrast, LST exhibits an increasing trend, highlighting intensifying urban heat island effects. The correlation analysis between NDVI and LST reveals a negative relationship (R² ≈ 0.10), indicating that areas with higher vegetation density tend to have lower surface temperatures. However, the relatively weak correlation suggests that additional factors, such as urban structure and land use patterns, also influence thermal dynamics. The findings demonstrate the importance of integrating vegetation indices and thermal data for urban ecological monitoring and provide valuable insights for sustainable urban planning and green infrastructure development.
Keywords
Urban green biomass, NDVI, EVI, Land Surface Temperature (LST), Urban Heat Island (UHI), Remote sensing, Google Earth Engine, Spatio-temporal analysis, Tashkent.
References
- Oke, T. R. (1982). The energetic basis of the urban heat island. Quarterly Journal of the Royal Meteorological Society, 108(455), 1–24.
- https://doi.org/10.1002/qj.49710845502
- Voogt, J. A., & Oke, T. R. (2003). Thermal remote sensing of urban climates. Remote Sensing of Environment, 86(3), 370–384.
- https://doi.org/10.1016/S0034-4257(03)00079-8
- Weng, Q. (2009). Thermal infrared remote sensing for urban climate and environmental studies: Methods, applications, and trends. ISPRS Journal of Photogrammetry and Remote Sensing, 64(4), 335–344.
- https://doi.org/10.1016/j.isprsjprs.2009.03.007
- Weng, Q., Lu, D., & Schubring, J. (2004). Estimation of land surface temperature–vegetation abundance relationship for urban heat island studies. Remote Sensing of Environment, 89(4), 467–483.
- https://doi.org/10.1016/j.rse.2003.11.005
- Rouse, J. W., Haas, R. H., Schell, J. A., & Deering, D. W. (1974). Monitoring vegetation systems in the Great Plains with ERTS. NASA Special Publication, 351, 309–317.
- Huete, A., Didan, K., Miura, T., Rodriguez, E. P., Gao, X., & Ferreira, L. G. (2002). Overview of the radiometric and biophysical performance of the MODIS vegetation indices. Remote Sensing of Environment, 83(1–2), 195–213.
- https://doi.org/10.1016/S0034-4257(02)00096-2
- Gill, S. E., Handley, J. F., Ennos, A. R., & Pauleit, S. (2007). Adapting cities for climate change: The role of green infrastructure. Built Environment, 33(1), 115–133.
- Zhou, W., Huang, G., & Cadenasso, M. L. (2011). Does spatial configuration matter? Understanding the effects of land cover pattern on land surface temperature. Landscape and Urban Planning, 102(1), 54–63.
- https://doi.org/10.1016/j.landurbplan.2011.03.009
- Li, X., Zhou, Y., Asrar, G. R., Imhoff, M., & Li, X. (2014). The surface urban heat island response to urban expansion. Environmental Research Letters, 9(7), 074015.
- https://doi.org/10.1088/1748-9326/9/7/074015
- Seto, K. C., Güneralp, B., & Hutyra, L. R. (2012). Global forecasts of urban expansion to 2030 and direct impacts on biodiversity and carbon pools. PNAS, 109(40), 16083–16088.
- https://doi.org/10.1073/pnas.1211658109
- Zhang, Y., Odeh, I. O. A., & Han, C. (2013). Bi-temporal characterization of land surface temperature in relation to impervious surface area. Remote Sensing of Environment, 113(7), 1466–1475.