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Delineating the climate change impacts on urban environment along with heat stress in the Indian tropical city

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dc.citedby0
dc.contributor.authorHalder B.en_US
dc.contributor.authorChatterjee P.en_US
dc.contributor.authorRana B.en_US
dc.contributor.authorBandyopadhyay J.en_US
dc.contributor.authorPande C.B.en_US
dc.contributor.authorAhmed K.O.en_US
dc.contributor.authorElkhrachy I.en_US
dc.contributor.authorRadwan N.en_US
dc.contributor.authorid57217238320en_US
dc.contributor.authorid59337413700en_US
dc.contributor.authorid58887957000en_US
dc.contributor.authorid57195753796en_US
dc.contributor.authorid57193547008en_US
dc.contributor.authorid57223260928en_US
dc.contributor.authorid55481426800en_US
dc.contributor.authorid56763877500en_US
dc.date.accessioned2025-03-03T07:41:29Z
dc.date.available2025-03-03T07:41:29Z
dc.date.issued2024
dc.description.abstractIndia experiences significant levels of temperature variance as a result of urbanization, deforestation, and industrial growth, all of which contribute to a progressive increase in heat island effects. Significant landform change has occurred in Bhubaneswar City, Odisha, in recent decades as a result of major plant loss and temperature unpredictability. Thus, during the summer and winter months, an examination of the long-term heat island impacts is essential for Bhubaneswar. The evolution of landforms and heat island impacts in Bhubaneswar are evaluated using Landsat images from 1991 to 2021 datasets and correlation analysis of heat islands and geospatial variables. Between 1991 and 2021 with a 10-year gap, the landforms studied showed an increase in built-up land (38.009 km2), a decrease in vegetation (13.875 km2), bare ground (16.306 km2), and water bodies (7.828 km2). The annual temperature variance in Bhubaneswar was 0.124 �C (summer), and 0.293 �C (winter). Surface temperatures varied by about 3.71 �C (summer) and 8.80 �C (winter). During the study years, heat islands increased from 2.89 to 4.27 (summer) and 2.30 to 3.87 (winter). In Bhubaneswar, there was an increase in ecological variation of 0.092 (summer), and 0.071 (winter). There is a statistically significant negative correlation between the R2 values and the temperature and the built-up indices. Using this dataset, administrative and development authorities can choose which measures to take to counteract the effects of variations in thermal variation. Finding out how man-made land use structures, industrial zones, and other areas contribute to the built-up area a direct consequence of heat islands was the aim of this study. ? 2024 Elsevier Ltden_US
dc.description.natureFinalen_US
dc.identifier.ArtNo103745
dc.identifier.doi10.1016/j.pce.2024.103745
dc.identifier.scopus2-s2.0-85204539532
dc.identifier.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85204539532&doi=10.1016%2fj.pce.2024.103745&partnerID=40&md5=3d8ca0d8947be94b4a661ef621deed1c
dc.identifier.urihttps://irepository.uniten.edu.my/handle/123456789/36164
dc.identifier.volume136
dc.publisherElsevier Ltden_US
dc.sourceScopus
dc.sourcetitlePhysics and Chemistry of the Earth
dc.subjectBhubaneswar
dc.subjectIndia
dc.subjectOdisha
dc.subjectBhubaneswar
dc.subjectClimate change impact
dc.subjectHeat island
dc.subjectHeat stress
dc.subjectIndustrial growth
dc.subjectLandform monitoring
dc.subjectTemperature variance
dc.subjectThermal
dc.subjectUrban environments
dc.subjectUrban heat island
dc.subjectclimate change
dc.subjectclimate effect
dc.subjectenvironmental monitoring
dc.subjectenvironmental stress
dc.subjectheat island
dc.subjectlandform evolution
dc.subjectregression analysis
dc.subjectsurface temperature
dc.subjecturban area
dc.subjectTropical cyclone
dc.titleDelineating the climate change impacts on urban environment along with heat stress in the Indian tropical cityen_US
dc.typeArticleen_US
dspace.entity.typePublication
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