2021
DOI: 10.1016/j.rsase.2021.100587
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Comparison of temporal changes in urban settlements and land surface temperature in Rangpur and Gazipur Sadar, Bangladesh after the establishment of city corporation

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Cited by 13 publications
(8 citation statements)
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“…Increased NDBI signifies increased build-ups of impervious surfaces or urbanization. As impervious surfaces show the highest temperatures in built-up areas [ 26 ], LST should be positively correlated with NDBI. Figure 4 (b) shows a substantial positive association between NDBI and LST in 2018, suggesting built-up areas increased in 2018 compared to 2000–2016, altering the thermal characteristics.…”
Section: Discussionmentioning
confidence: 99%
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“…Increased NDBI signifies increased build-ups of impervious surfaces or urbanization. As impervious surfaces show the highest temperatures in built-up areas [ 26 ], LST should be positively correlated with NDBI. Figure 4 (b) shows a substantial positive association between NDBI and LST in 2018, suggesting built-up areas increased in 2018 compared to 2000–2016, altering the thermal characteristics.…”
Section: Discussionmentioning
confidence: 99%
“…Due to increasing urbanization, land surface types have been changing in recent years [ 25 ]. Using remotely sensed satellite imagery, a change in surface temperature may be observed, which is an indicator of impervious surface build-up [ 26 ]. The distribution of LST is greatly influenced by the presence of natural vegetation [ 15 , 27 , 28 , 29 ].…”
Section: Introductionmentioning
confidence: 99%
“…To achieve this global goal and frame policies for mitigating Urban climate (UC) and Urban microclimate (UMC) change it is crucial to understand the Multi-Temporal LULC change and its impact on LST. Several studies have used Remote Sensing and GIS to study LST its impact on UC [15][16][17][18][19]. To carry out Multi Spatio-Temporal study of UMC using Remote Sensing is challenging with the constraints of proprietary software, big data, computer space, and tedious hour of processing data.…”
Section: Introductionmentioning
confidence: 99%
“…The urban growth impacts the carbon cycle through land cover change, modification of surface energy balance especially albedo, and the loss of carbon stocks. Increasing trends in urban impervious surface have negative environmental impacts to the city climate as, less precipitation, more dryness and urban higher temperatures and associated natural hazards related to heat waves and urban heat islands 6,7 . However, the response of urban vegetation land cover to multiple climatic stressors varies interannually and in different seasons of the years, related to different vegetation type's characteristics and climatic conditions.…”
Section: Introductionmentioning
confidence: 99%