Analysis of Land Surface Temperatures in the "Local Climate Zones" of Novi Sad (Serbia)

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F20%3A73604028" target="_blank" >RIV/61989592:15310/20:73604028 - isvavai.cz</a>
Result on the web
<a href="http://www.glasniksgd.rs/index.php/home/article/view/716/pdf" target="_blank" >http://www.glasniksgd.rs/index.php/home/article/view/716/pdf</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.2298/GSGD2001041S" target="_blank" >10.2298/GSGD2001041S</a>

Result language
angličtina
Original language name
Analysis of Land Surface Temperatures in the "Local Climate Zones" of Novi Sad (Serbia)
Original language description
In this study, the Local Climate Zones (LCZs) in Novi Sad, the second largest city in Serbia, are analysed as to surface temperature differences. The LCZs were delineated on the basis of the GIS-based method created by Geletič & Lehnert (2016). Land Surface Temperatures (LSTs) were derived from the satellites Terra, sensor ASTER, and LANDSAT-8. The thermal images were provided at a similar time (at about 9.30 AM) between 2002 and 2008 (ASTER) and between 2013 and 2017 (LANDSAT-8). Statistical analyses, including the analysis of variance (ANOVA) and Tukey-HSD test, were employed to reveal LST differences between the LCZs. The results indicate that in 84% of cases there were significant differences in LST between pairs of LCZs. Temperature differences between LCZs were the most pronounced in the summer season. In general, 8 (large low-rise), 10 (heavy industry), 2 (compact midrise) and 3 (compact low-rise) LCZs had the highest surface temperatures in Novi Sad. Contrary to this, LCZs A (dense trees), B (scattered trees) G (water bodies) were the coolest zones.
Czech name
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Czech description
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Publication year
2020
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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