Inter-Seasonal Variations of Surface Temperature in the Urbanized Environment of Delhi Using Landsat Thermal Data
Complex land use/cover patterns in urban areas significantly influence their prevailing surface temperature conditions. As a result of differential cooling and heating of various land use/cover, large temperature ranges are associated with bare land, built-up land, etc. and low ranges are found in v...
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doaj-4640cfc948b149fa8eb9cc954cd12d502020-11-25T00:08:38ZengMDPI AGEnergies1996-10732014-03-01731811182810.3390/en7031811en7031811Inter-Seasonal Variations of Surface Temperature in the Urbanized Environment of Delhi Using Landsat Thermal DataRam Babu Singh0Aakriti Grover1Jinyan Zhan2Department of Geography, Delhi School of Economics, University of Delhi, Delhi 110007, IndiaDepartment of Geography, Swami Shraddhanand College, University of Delhi, Delhi 110036, IndiaState Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875, ChinaComplex land use/cover patterns in urban areas significantly influence their prevailing surface temperature conditions. As a result of differential cooling and heating of various land use/cover, large temperature ranges are associated with bare land, built-up land, etc. and low ranges are found in vegetation cover and water bodies. Extremely high and low temperature conditions in built-up land have direct and negative impacts on health conditions, and therefore are imperative to study. Thus, an attempt has been made in this research to analyze seasonal variations in surface temperature in city of Delhi. Landsat Thematic Mapper (TM) 5 satellite images for the four seasons, viz., 16 January (winter), 5 March (spring), 8 May (summer) and 29 September (autumn) 2011 have been used to interpret the distribution and changes in surface temperature. A total of 80 samples from all land use/cover categories were taken to generalize the patterns along with north-south and west-east profiles. The extracted surface temperature patterns reflect the spatial and temporal dynamics of temperature over different land use/cover. The north-south and west-east gradient of temperature demonstrates that the core of Delhi has a much lower temperature and weak urban heat island (UHI) phenomenon.http://www.mdpi.com/1996-1073/7/3/1811Delhiseasonal variationmicro climateurban heat island (UHI)land use/cover |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Ram Babu Singh Aakriti Grover Jinyan Zhan |
spellingShingle |
Ram Babu Singh Aakriti Grover Jinyan Zhan Inter-Seasonal Variations of Surface Temperature in the Urbanized Environment of Delhi Using Landsat Thermal Data Energies Delhi seasonal variation micro climate urban heat island (UHI) land use/cover |
author_facet |
Ram Babu Singh Aakriti Grover Jinyan Zhan |
author_sort |
Ram Babu Singh |
title |
Inter-Seasonal Variations of Surface Temperature in the Urbanized Environment of Delhi Using Landsat Thermal Data |
title_short |
Inter-Seasonal Variations of Surface Temperature in the Urbanized Environment of Delhi Using Landsat Thermal Data |
title_full |
Inter-Seasonal Variations of Surface Temperature in the Urbanized Environment of Delhi Using Landsat Thermal Data |
title_fullStr |
Inter-Seasonal Variations of Surface Temperature in the Urbanized Environment of Delhi Using Landsat Thermal Data |
title_full_unstemmed |
Inter-Seasonal Variations of Surface Temperature in the Urbanized Environment of Delhi Using Landsat Thermal Data |
title_sort |
inter-seasonal variations of surface temperature in the urbanized environment of delhi using landsat thermal data |
publisher |
MDPI AG |
series |
Energies |
issn |
1996-1073 |
publishDate |
2014-03-01 |
description |
Complex land use/cover patterns in urban areas significantly influence their prevailing surface temperature conditions. As a result of differential cooling and heating of various land use/cover, large temperature ranges are associated with bare land, built-up land, etc. and low ranges are found in vegetation cover and water bodies. Extremely high and low temperature conditions in built-up land have direct and negative impacts on health conditions, and therefore are imperative to study. Thus, an attempt has been made in this research to analyze seasonal variations in surface temperature in city of Delhi. Landsat Thematic Mapper (TM) 5 satellite images for the four seasons, viz., 16 January (winter), 5 March (spring), 8 May (summer) and 29 September (autumn) 2011 have been used to interpret the distribution and changes in surface temperature. A total of 80 samples from all land use/cover categories were taken to generalize the patterns along with north-south and west-east profiles. The extracted surface temperature patterns reflect the spatial and temporal dynamics of temperature over different land use/cover. The north-south and west-east gradient of temperature demonstrates that the core of Delhi has a much lower temperature and weak urban heat island (UHI) phenomenon. |
topic |
Delhi seasonal variation micro climate urban heat island (UHI) land use/cover |
url |
http://www.mdpi.com/1996-1073/7/3/1811 |
work_keys_str_mv |
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