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- W4376479434 abstract "The urban heat island (UHI) is formed due to higher local temperatures in urban areas than surrounding rural areas. Impervious surfaces and vegetation are the two major land covers that have the capability to modify energy fluxes. The Latent Heat flux, Sensible Heat Flux and the Ground Heat flux was obtained for Bangalore city and ratio of fluxes to net radiation was calculated. The mean of ratio of each flux to net radiation was calculated for each land cover and found that the urban and bare soil region shows higher values of <tex xmlns:mml=http://www.w3.org/1998/Math/MathML xmlns:xlink=http://www.w3.org/1999/xlink>$mathrm{G}/mathrm{R}_{mathrm{n}}$</tex> as compared to the vegetated land covers. The urban land cover showed higher values of <tex xmlns:mml=http://www.w3.org/1998/Math/MathML xmlns:xlink=http://www.w3.org/1999/xlink>$mathrm{H}/mathrm{R}_{mathrm{n}}$</tex> as compared to the natural land covers and the vegetation and waterbody showed higher values of <tex xmlns:mml=http://www.w3.org/1998/Math/MathML xmlns:xlink=http://www.w3.org/1999/xlink>$text{LE}/mathrm{R}_{mathrm{n}}$</tex> than other land covers. The relation of sensible heat flux with imperviousness and latent heat flux with vegetation was determined. The plot of <tex xmlns:mml=http://www.w3.org/1998/Math/MathML xmlns:xlink=http://www.w3.org/1999/xlink>$mathrm{H}/mathrm{R}_{mathrm{n}}$</tex> with ISF and <tex xmlns:mml=http://www.w3.org/1998/Math/MathML xmlns:xlink=http://www.w3.org/1999/xlink>$text{LE}/mathrm{R}_{mathrm{n}}$</tex> with NDVI, both showed good positive relation." @default.
- W4376479434 created "2023-05-14" @default.
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- W4376479434 date "2022-12-01" @default.
- W4376479434 modified "2023-10-04" @default.
- W4376479434 title "Assessment of Surface Energy Fluxes variation with Land Cover Parameters using LandSat Satellite data" @default.
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- W4376479434 doi "https://doi.org/10.23919/ursi-rcrs56822.2022.10118439" @default.
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