Sustainable Development Practices Using Geoinformatics. Группа авторов

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etc., as the observations collected from the ground cannot provide much detailed information over a larger area (Wu et al., 2015). LST is the temperature radiated by the surface and measured within limited boundary of lower atmosphere from the surface, which is proportionally dependent on land surface emissivity (Wan and Dozier 1996; Wang et al., 2015; Isaya Ndossi and Avdan 2016). The LST is technically different from the Atmospheric temperature and is largely affected by the urban canopy layer. LST calculation was done with the help of Inversion of Planck’s Function (Isaya Ndossi and Avdan 2016; Zhang, Wang, and Li 2006; Srivastava et al., 2014; Artis and Carnahan 1982; Sobrino, Caselles, and Becker 1990). The formula for LST calculation (Eq. 1.2) is as follows:

      where Ts = land surface temperature (°C), BT = brightness temperature (K), λ = wavelength of the emitted radiance, ρ = (h * c/σ) = 1.438 *10−2mK, and ε = land surface emissivity

      The results of the data analyzed for this study are discussed in four sections.

An illustration of the Land Use and Land Cover map of Barasat municipality of the years 2001, 2011, and 2017.
Class Name Area in %
2001 2011 2017
Bare land 16.70 13.39 8.25
Water body 2.40 2.36 1.47
Agricultural fallow 7.92 4.75 3.74
Built-up area 6.79 16.38 29.23
Built-up with green space 38.20 40.79 45.80
Green space 27.99 22.33 11.50

      1.4.2 Urban Sprawl

An illustration of the Urban Sprawl pattern from 2001 to 2017. The figure has two schematic illustrations. (A) The Circular pattern of increasing population from center of the city. (B) The Linear pattern of increasing population alongside road.

      1.4.3 Impact of Urban Sprawl on Vegetation Cover

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